Skocz do pozycji: 1.

Tytuł:

The stratigraphy of the Oligocene deposits from the Ropa tectonic window (Grybów Nappe, Western Carpathians, Poland)

Autorzy:

Oszczypko-Clowes, M.

Powiązania:

https://bibliotekanauki.pl/articles/2060226.pdf

Data publikacji:

2008

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Western Carpathians
Oligocene
calcareous nannoplancton

Opis:

The Ropa tectonic window of the Magura Nappe is composed of Oligocene deposits that belong to the Grybów Nappe. The youngest deposits of the Ropa tectonic window are correlated with calcareous nannoplanton zones NP24 and NP25. The NP24 zone interval was determined in the Sub-Grybów Beds and in the Grybów Marl Formation, whereas the Krosno (Cergowa) Beds belong to zone NP25. This age determination corresponds well with that of other Magura Nappe tectonic windows and also with the southern part of the Silesian and Dukla nappes. The facies and age of the Krosno Beds from the Grybów succession record the termination of Fore-Magura basins. The Grybów Nappe deposits in the Ropa tectonic window are overthrust by Cretaceous-Eocene formations of the Magura Nappe.

Źródło:

Geological Quarterly; 2008, 52, 2; 127-127
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:

Pseudothurmanniid ammonites from quarries near Lietavská Lúčka and their stratigraphical significance (Late Hauterivian, Central Western Carpathians, Slovakia)

Autorzy:

Vašiček, Z.
Malek, O.

Powiązania:

https://bibliotekanauki.pl/articles/2060607.pdf

Data publikacji:

2017

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

ammonites
taxonomy
stratigraphy
Hauterivian
Western Carpathians

Opis:

Pseudothurmanniid ammonites within Upper Hauterivian calcareous deposits are present in quarries on Polomec Hill near the village of Lietavská Lúčka, Slovakia. These deposits belong to the Mráznica Formation of the Krížna Nappe that is a part of the Fatricum Unit in the Central Western Carpathians. Nine ammonite species are described in detail, one of which, Binellicerasmichalíki, is new. The species identified indicate the Upper Hauterivian Balearis and Ohmi ammonite zones. The zone of the uppermost Hauterivian, Catulloi Zone, is not documented as far as pseudothurmanniid ammonites are concerned. The lackof developmentally younger representatives of the pseudothurmanniid ammonites neitherin the studied locali ty, nor in other Slovak locali ties, is explained by marked changes in the northern Tethyan margin in Europe duri ng the latest Hauterivian.

Źródło:

Geological Quarterly; 2017, 61, 3; 613--631
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 3.

Tytuł:

A new synthesis of the geological structure of Slovakia - the general geological map at 1:200 000 scale

Autorzy:

Bezák, V.
Biely, A.
Elećko, M.
Konećny, V.
Mello, J.
Polák, M.
Potfaj, M.

Powiązania:

https://bibliotekanauki.pl/articles/2059015.pdf

Data publikacji:

2011

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Slovakia
Western Carpathians
geological structures
general

Opis:

Systematic geological mapping of the Slovak Republic territory over the last forty years, when many regional geological maps at 1:50 000 scale were issued, culminated in 2008 and 2009 in a new synthesis of the geological structure of the Western Carpathians on the Slovak territory in the form of a general geological map at 1:200 000 scale. An integral part of this activity was the solving of interregional correlation problems, a settled of tectonic classification of the Western Carpathians as well as a specification of the lithostratigraphical content of the tectonic units. The results of this synthesis are described in this contribution - a brief review of the principal geological units of the Western Carpathians that are depicted in the tectonic interpretation and in the geological sections. The Western Carpathians are geologically divided into the Outer (Flysch Belt) and Inner (Inner Carpathian Block). These two zones are products of the youngest, mainly Neogene Neo-Alpine tectonic activity. Separating the two zones is a tectonic structure - the Klippen Belt -which contains elements from both. The Inner Carpathian Block possesses a Palaeoalpine tectonic pattern composed of crustal tectonic units and superficial nappes. The crustal units are composed of the crystalline basement and its Upper Paleozoic and Mesozoic cover. The basement consists of fragments of Hercynian tectonic units from the Paleozoic phase of crustal evolution. The superficial nappes comprise mostly upper Paleozoic and Mesozoic sequences. Cenozoic deposits and volcanic rocks are deposited on the Palaeoalpine nappe structure.

Źródło:

Geological Quarterly; 2011, 55, 1; 1-8
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 4.

Tytuł:

Field mapping of buried faults : a new approach applied in the Western Carpathians

Autorzy:

Marko, F.
Dyda, M.
Gajdoš, V.
Rozimant, K.
Mojzeš, A.

Powiązania:

https://bibliotekanauki.pl/articles/2059816.pdf

Data publikacji:

2015

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

faults
geophysical survey
dowsing
Western Carpathians

Opis:

Fault array in an area covered by Quaternary sediments and deprived of bedrock outcrops was investigated using fault trace mapping by geophysical methods and human feedback information from dowsing. The tectonics in the study area is dominated by a ENE-WSW fault zone affecting regional-scale structures. The fault network was approximated by dowsing-enhanced mapping and subsequently confirmed by field geophysical measurements using electromagnetic and radon emanometry methods. A resultant detailed map of structural discontinuities highlighted that combined dowsing and geophysical survey is an effective and reliable tool to identify buried faults. This approach with its low costs and fast field recognition is highly recommended for construction-work planning and for mineral resources exploration and exploitation.

Źródło:

Geological Quarterly; 2015, 59, 1; 35--46
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 5.

Tytuł:

Early Cretaceous ammonites and dinoflagellates from the Western Tatra Mountains, Poland

Autorzy:

Vasicek, Z.
Błażejowski, B.
Gaździcki, A.
Król, M.
Lefeld, J.
Skupień, P.
Wierzbowski, A.

Powiązania:

https://bibliotekanauki.pl/articles/2082277.pdf

Data publikacji:

2020

Wydawca:

Polska Akademia Nauk. Instytut Paleobiologii PAN

Tematy:

Ammonoidea
Anomiidae
Dinoflagellata
Valanginian
Hauterivian
Western Carpathians

Opis:

The first Early Cretaceous (Valanginian–Hauterivian) ammonite fauna from the lower part of the Kościeliska Marl Formation (Wściekły Żleb Member) of the Lower Sub-Tatric (Krížna) Nappe, in the Lejowa Valley of the Tatra Mountains are described. The fauna is precisely placed in the succession and consists of five species: Olcostephanus densicostatus, Spitidiscus cf. cankovi, Criosarasinella cf. subheterocostata, Crioceratites primitivus, and Crioceratites coniferus and additionally an aptychus Didayilamellaptychus seranonis. Remarkable are the valves of anomiid bivalves attached to body chamber of large size heteromorph ammonite C. primitivus. Moreover, a variety of stratigraphically important organic-walled dinoflagellate cysts are recovered from this locality. Dinoflagellates: Cymososphaeridium validum, Circulodinium vermiculatum, and representatives of Bourkidinium define the Upper Valanginian–Lower Hauterivian Sentusidinium sp. A Dinocyst Subzone of the Cymososphaeridium validum Zone. The character of deposits, the palynofacies, and associations of dinoflagellate cysts indicate a calm marine outer neritic environment.

Źródło:

Acta Palaeontologica Polonica; 2020, 65, 4; 799-810
0567-7920

Pojawia się w:

Acta Palaeontologica Polonica

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 6.

Tytuł:

Genesis and stability of accessory phosphates in silicic magmatic rocks: a Western Carpathian case study

Autorzy:

Broska, Igor
Perik, Igor

Powiązania:

https://bibliotekanauki.pl/articles/2086521.pdf

Data publikacji:

2008

Wydawca:

Polskie Towarzystwo Mineralogiczne

Tematy:

phosphates
monazite
apatite
xenotime
granite
Western Carpathians

Opis:

The formation of accessory phosphates in granites reflects many chemical and physical factors, including magma composition, oxidation state, concentrations of volatiles and degree of differentiation. The geotectonic setting of granites can be judged from the distribution and character of their phosphates. Robust apatite crystallization is typical of the early magmatic crystallization of I-type granitoids, and of late magmatic stages when increased Ca activity may occur due to the release of anorthite from plagioclase. Although S-type granites also accumulate apatite in the early stages, increasing phosphorus in late differentiates is common due to their high ASI. The apatite from the S-types is enriched in Mn compared to that in I-type granites. A-type granites characteristically contain minor amounts of apatite due to low P concentrations in their magmas. Monazite is typical of S-type granites but it can also become stable in late I-type differentiates. Huttonite contents in monazite correlate roughly positively with temperature. The cheralite molecule seems to be highest in monazite from the most evolved granites enriched in B and F. Magmatic xenotime is common mainly in the S-type granites, but crystallization of secondary xenotime is not uncommon. The formation of the berlinite molecule in feldspars in peraluminous melts may suppress phosphate precipitation and lead to distributional inhomogeneities. Phosphate mobility commonly leads to the formation of phosphate veinlets in and outside granite bodies. The stability of phosphates in the superimposed, metamorphic processes is restricted. Both monazite-(Ce) and xenotime-(Y) are unstable during fluid-activated overprinting. REE accessories, especially monazite and allanite, show complex replacement patterns culminating in late allanite and epidote formation.

Źródło:

Mineralogia; 2008, 39, 1/2; 53--65
1899-8291
1899-8526

Pojawia się w:

Mineralogia

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 7.

Tytuł:

Early Berriasian ammonites from the Štramberk Limestone in the Kotouč Quarry (Outer Western Carpathians, Czech Republic)

Autorzy:

Vašíček, Z.
Skupien, P.

Powiązania:

https://bibliotekanauki.pl/articles/191726.pdf

Data publikacji:

2013

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

ammonites
Berriasian
Štramberk area
Outer Western Carpathians

Opis:

Over 100 ammonites were collected from a block of bedded shallow-water Štramberk Limestone at a new location at the Kotouč Quarry, near Štramberk (Silesian Unit, Czech Republic). Berriaselline neocomitids, including Berriasella jacobi, B. oppeli, Tirnovella allobrogensis, T. cf. allobrogensis, Delphinella consanguinea, Pseudosubplanites cf. grandis and Malbosiceras cf. asper, are the most abundant species in this ammonite association. The olcostephanitid, Spiticeras blancheti, is rare. The index species for the Early Berriasian, B. jacobi, occurs in large numbers. On the basis of the present study, the upper boundary of the stratigraphic range of the Štramberk Limestone in the type area is dated as early Berriasian (ammonite Berriasella jacobi Zone). Ammonites with ages younger than early Berriasian have never been found in the Štramberk area. The deposition of the Štramberk Limestone in the Štramberk area came to an end during that period.

Źródło:

Annales Societatis Geologorum Poloniae; 2013, 83, 4; 329-342
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 8.

Tytuł:

Last scene in the large scale rotations of the Western Carpathians as reflected in paleomagnetic constraints

Autorzy:

Márton, Emö

Powiązania:

https://bibliotekanauki.pl/articles/184758.pdf

Data publikacji:

2020

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

Western Carpathians
large scale rotations
paleomagnetic constraints

Opis:

This paper provides an overview of the paleomagnetic results which constrain the post-Paleogene tectonic development of the Western Carpathians. A group of these results are relevant to the last stage of the Tertiary folding and thrusting of the Silesian, Dukla and Magura nappes of the Outer Western Carpathian and were obtained from Paleogene-Lower Miocene flysch sediments. Both the pre- and post-folding remanences indicate about 50° CCW vertical axis rotation with respect to the present orientation. This is about a 60° rotation relative to stable Europe. It follows that the general orientation of the Silesian and more internal nappes were NW-SE, at least until the mid-Miocene. The CCW vertical axis rotation was coordinated with that of the Central Carpathian Paleogene Basin. The termination of the rotation can be estimated from the paleomagnetic data available from the Pieniny andesites which intruded the Pieniny Klippen Belt and the southern part of the Magura Nappe as well as from those obtained for the Neogene intramontane basins which opened up in the Outer and in the Central Western Carpathians. The paleomagnetic vectors for the andesites form two groups. The first group suggests about 45° CCW rotation relative to north, while the second shows no rotation. At the present stage of our knowledge it seems likely that some of the andesite bodies were intruded around 18 Ma, which is the oldest isotope age for the intrusions of the Wżar Mts, while some other bodies could have been emplaced after the rotation, around 11 Ma, which is the youngest isotope age for the Brijarka quarry. Vertical axis CCW rotation was also observed on sediments older than 11.6 Ma in the Orava-Nowy Targ Intramontane Basin which saddles the Magura Nappe and the Central Carpathian Paleogene Basin. However, this rotation was related to fault zone activity and was not attributed to the general rotation of the Outer Western Carpathian nappe system. Paleomagnetic results from the Nowy Sącz Intramontane Basin, which opened over the Magura Nappe, and those for the Central Western Carpathian Turiec Intramontane Basin do not indicate vertical axis rotation. In the first case, the loosely controlled age limit of the termination of the rotation is around 12 Ma. Well constrained results from the second basin imply that the rotation was definitely over by 8 Ma. Based on the above observations, and aware of the problem of often loose age control on the formation and deformation of the deposits of the intramontane basins, it is tentatively concluded that the large scale CCW rotation of the Central Western Carpathians, together with the Magura, Dukla and Silesian nappes, must have started after 18 Ma and terminated around 11 Ma.

Źródło:

Geology, Geophysics and Environment; 2020, 46, 2; 109-133
2299-8004
2353-0790

Pojawia się w:

Geology, Geophysics and Environment

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 9.

Tytuł:

Evidence for differential crustal uplift between the neighbouring Kamienica and Ochotnica river valleys in the Polish Outer Western Carpathians

Autorzy:

Olszak, J.

Powiązania:

https://bibliotekanauki.pl/articles/191477.pdf

Data publikacji:

2009

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

strath terraces
neotectonics
Outer Western Carpathians
Polska

Opis:

Young tectonic movements in the Carpathians, both vertical and horizontal ones, display local varia- tions. The Dunajec River valley is one of the areas where this differentiation has been documented best. New data on differentiated tectonic uplift, based on the study of changing elevations of five levels of fluvial strath terraces, were obtained in the lowermost reaches of two Dunajec’s tributaries: Kamienica and Ochotnica. The results indicate a change in the rate of valley bottom incision during the Pleistocene. Initially, the rate of incision was higher in the Kamienica River valley during ca. 600–350 ka BP. Later, since ca. 130 ka BP until now, the proportion became reversed and the rate of incision was nearly twice as fast in the Ochotnica River valley than in the Kamienica River valley. This is probably related to the mobility of the overthrust of the Krynica slice onto the Bystrica slice, both building the inner portion of the Magura Nappe. Reactivation of this thrust may be a result of neotectonic activity of large-scale faults situated at the depths of 5–20 km and possibly rooted in the Palaeozoic– Mesozoic basement.

Źródło:

Annales Societatis Geologorum Poloniae; 2009, 79, No 2; 187-193
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 10.

Tytuł:

Morphology of Czarna Cave and its significance for the geomorphic evolution of the Kościeliska Valley (Western Tatra Mts)
Morfologia Jaskini Czarnej i jej znaczenie dla geomorfologicznego rozwoju Doliny Kościeliskiej

Autorzy:

Gradziński, M.
Kicińska, D.

Powiązania:

https://bibliotekanauki.pl/articles/191558.pdf

Data publikacji:

2002

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

scallops
cave development
karst hydrology
Western Carpathians

Opis:

Czarna Cave represents phreatic cave with multiple loops. No cave level developed at the water table was detected. The cave was later modified by invasion vadose waters and breakdown processes. The phreatic paleoflow directions were analyse from the asymmetry of scallops. The paleoflow was directed from the east to the west, that is in a direction of the Kościeliska Valley. Therefore, this valley represented the main discharge zone of the region during the formation of Czarna Cave.

Źródło:

Annales Societatis Geologorum Poloniae; 2002, 72, No 3; 255-62
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 11.

Tytuł:

„Depositional setting of the Oligocene sequence of the Western Carpathians in the Polish Spisz region : a reinterpretation based on integrated palynofacies and sedimentological analyses” – Reply

Autorzy:

Filipek, A.
Wysocka, A.
Barski, M.

Powiązania:

https://bibliotekanauki.pl/articles/2060460.pdf

Data publikacji:

2018

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Oligocene sequence
Western Carpathians
palynofacies
sedimentological analyses

Opis:

[...]First of all, we would like to note that our reply will concentrate on substantial comments on the presented results or/and questionable interpretations.[...]

Źródło:

Geological Quarterly; 2018, 62, 3; 751--754
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 12.

Tytuł:

Western Carpathians in the territory of the Czech Republic

Autorzy:

Skupien, P.
Vasicek, Z.

Powiązania:

https://bibliotekanauki.pl/articles/184033.pdf

Data publikacji:

2008

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

Karpaty Zachodnie
Czechy
Western Carpathians
Czech Republic

Źródło:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2008, 34, 3/1; 139-149
0138-0974

Pojawia się w:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 13.

Tytuł:

Genesis and stability of accessory phosphates in silicic magmatic rocks: a Western Carpathian case study

Autorzy:

Broska, I.
Perik, I.

Powiązania:

https://bibliotekanauki.pl/articles/2086551.pdf

Data publikacji:

2008

Wydawca:

Polskie Towarzystwo Mineralogiczne

Tematy:

phosphates
monazite
apatite
xenotime
granite
Western Carpathians

Opis:

The formation of accessory phosphates in granites reflects many chemical and physical factors, including magma composition, oxidation state, concentrations of volatiles and degree of differentiation. The geotectonic setting of granites can be judged from the distribution and character of their phosphates. Robust apatite crystallization is typical of the early magmatic crystallization of I-type granitoids, and of late magmatic stages when increased Ca activity may occur due to the release of anorthite from plagioclase. Although S-type granites also accumulate apatite in the early stages, increasing phosphorus in late differentiates is common due to their high ASI. The apatite from the S-types is enriched in Mn compared to that in I-type granites. A-type granites characteristically contain minor amounts of apatite due to low P concentrations in their magmas. Monazite is typical of S-type granites but it can also become stable in late I-type differentiates. Huttonite contents in monazite correlate roughly positively with temperature. The cheralite molecule seems to be highest in monazite from the most evolved granites enriched in B and F. Magmatic xenotime is common mainly in the S-type granites, but crystallization of secondary xenotime is not uncommon. The formation of the berlinite molecule in feldspars in peraluminous melts may suppress phosphate precipitation and lead to distributional inhomogeneities. Phosphate mobility commonly leads to the formation of phosphate veinlets in and outside granite bodies. The stability of phosphates in the superimposed, metamorphic processes is restricted. Both monazite-(Ce) and xenotime-(Y) are unstable during fluid-activated overprinting. REE accessories, especially monazite and allanite, show complex replacement patterns culminating in late allanite and epidote formation.

Źródło:

Mineralogia; 2008, 39, 1/2; 53--65
1899-8291
1899-8526

Pojawia się w:

Mineralogia

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 14.

Tytuł:

Magnetostratigraphy of the Oligocene Lower Krosno Beds from the Hulskie section (Outer Carpathians in Poland)

Autorzy:

Nawrocki, J.
Malata, T.
Rosowiecka, O.

Powiązania:

https://bibliotekanauki.pl/articles/2060521.pdf

Data publikacji:

2016

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Outer Western Carpathians
Krosno Beds
Jasło limestone
magnetostratigraphy

Opis:

The Oligocene flysch sequence from the Hulskie section in the Polish Outer Carpathians was palaeomagnetically examined. The flysch complex containing the Jasło and Zagórze limestone horizons revealed palaeomagnetic properties sufficient for a magnetostratigraphy to be established. The correlation of the local to the global magnetic polarity scale indicates that the Jasło limestone was deposited very close to the Rupelian and Chattian boundary i.e. ca. 28.4 Ma. In the same way, the age of the Zagórze limestone was defined as close to ca. 27.6 Ma. The entire450 mof studied section was formed between ca. 29 and 26.5 Ma. It implies an average sedimentary ratio of about 18 cm per thousand years. The palaeomagnetic directions from the Hulskie section do not display the Fisher type distribution and do not fit the reversal test and therefore cannot be used for any regional tectonic reconstruction.

Źródło:

Geological Quarterly; 2016, 60, 4; 935--942
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 15.

Tytuł:

Assessment of landslide hazard from tree-ring eccentricity and from compression wood : a comparison

Autorzy:

Łuszczyńska, Katarzyna
Malik, Ireneusz
Wistuba, Małgorzata
Krąpiec, Marek

Powiązania:

https://bibliotekanauki.pl/articles/2058669.pdf

Data publikacji:

2019

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

eccentric growth
reaction wood
landslide activity
Western Carpathians

Opis:

We have compared maps of landslide activity and hazard, developed with the use of two different dendrochronological indicators: tree-ring eccentricity and reaction (compression) wood. The maps were prepared based on 125 Norway spruce (Picea abies L. Karst.) trees growing at 44 sampling points, distributed over an area of 3.75 km2. In general, the two maps show similar patterns of landslide activity. However, tree-ring eccentricity yielded a greater number of dated events (246) compared to compression wood (129). Besides the differences in the absolute values of dating results, the general landslide activity and hazard zonation based on both disturbances are similar. Both growth disturbances develop as a result of stem tilting. Eccentricity develops after slight tilting, while compression wood is developed when tilting is more significant. Because of the differences in the strength of disturbing factors, which cause the development of compression wood and growth eccentricity, the best approach would be to combine the results of dating obtained from the two methods. The dendrochronological analysis of tree growth disturbances (eccentric growth and compression wood) is a promising approach for determining landslide hazards in forested mountain areas and can be applied in spatial management.

Źródło:

Geological Quarterly; 2019, 63, 2; 296--301
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 16.

Tytuł:

Biostratigraphy and palaeoenvironment of the Kimmeridgian-Lower Tithonian pelagic deposits of the Krížna Nappe, Lejowa Valley, Tatra Mts. (southern Poland)

Autorzy:

Jach, R.
Řeháková, D.
Uchman, A.

Powiązania:

https://bibliotekanauki.pl/articles/2060506.pdf

Data publikacji:

2012

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

microfacies
biostratigraphy
calcareous dinoflagellates
calpionellids
Upper Jurassic
Western Carpathians

Opis:

The Upper Jurassic strata of the Krížna Unit in the Tatra Mts. comprises pelagic, fine-grained and well-oxygenated deposits. They are represented by red radiolarites and radiolarian limestones (Czajakowa Radiolarites Formation), red nodular limestones (Czorsztyn Limestones Formation) and wavy, platy or nodular light grey and reddish limestones and marlstones (Jasenina Formation). These deposits are mainly wackestones characterized by a succession of the following microfacies: radiolarian, filament-Saccocoma, Saccocoma and Globochaete–Saccocoma. The section comprises four calcareous dinoflagellate zones, i.e. the Late Kimmeridgian Moluccana Zone, and the Early Tithonian Borzai, Pulla and Malmica zones. In the uppermost part of the studied section, the Early Tithonian Dobeni Subzone of the Chitinoidella Zone has been identified. Using these biostratigraphic data, the sedimentation rate for the Late Kimmeridgian (Borzai Zone) and Early Tithonian (Dobeni Subzone of the Chitinoidella Zone) interval is estimated as 3.7 m/my. This is in accordance with the general trend of increasing sedimentation rate through the Tithonian and Berriasian. The increased supply of clastic material in the Jasenina Formation may have been caused by climate changes and continental weathering. The sedimentation was controlled mainly by eustatic changes and fluctuations in ACD and CCD levels.

Źródło:

Geological Quarterly; 2012, 56, 4; 773--788
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 17.

Tytuł:

Petrology and palaeotectonic setting of Cretaceous alkaline basaltic volcanismin the Pieniny Klippen Belt (Western Carpathians, Slovakia)

Autorzy:

Spišiak, J.
Plašienka, D.
Bucová, J.
Mikuš, T.

Powiązania:

https://bibliotekanauki.pl/articles/2059013.pdf

Data publikacji:

2011

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Western Carpathians
Pieniny Klippen Belt
Cretaceous
melanephelinite
petrology
geochemistry

Opis:

Occurrences of mafic alkaline volcanics are scattered all around Europe, being mostly related to anorogenic, extensional tectonic environments. While the widespread Cenozoic alkaline basalts have been intensively studied and are comparatively well-known, their Cretaceous precursors were often associated with the Alpine-Carpathian orogenic zones, and so their genesis and geodynamic setting are partially obscured by superimposed deformation and alteration. We describe a newly discovered body of melanephelionites inserted within the Upper Cretaceous deep-marine pelagic succession of the Pieniny Klippen Belt in Western Slovakia. The body consists of hyaloclastic lavas of nephelinitic composition. The mineralogical composition and geochemical features of the Vršatec volcanites correspond to melanephelinites. Reconstruction of the geodynamic setting of the Cretaceous mafic alkaline volcanism in the Alpine-Carpathian-Pannonian realm infers a general extensional/rifting tectonic regime that ultimately led to the opening of Penninic oceanic rift arms. However, this rifting started as basically passive and non-volcanic. Only during the later, post-breakup extension phases did the slow-spreading oceanic ridges develop, which are characterized by the MORB-type (mid-ocean-ridge basin) basaltic volcanism. Alkaline volcanic provinces have a linear character and appear to follow passive continental margins of Penninic oceanic arms opened during the Jurassic and Early Cretaceous. We infer that alkaline volcanism resulted from heating and partial melting of the subcontinental mantle lithosphere on the peripheries of asthenospheric upwellings confined to slow-spreading ridges of the Alpine Tethys. Consequently, regarding the debate about the plume vs. non-plume origin of the Cretaceous alkaline volcanism, the geological data from this area rather support the latter affinity.

Źródło:

Geological Quarterly; 2011, 55, 1; 27-48
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 18.

Tytuł:

Contrasting tectonic styles of the western and eastern parts of the Western Carpathian Klippen Belt in Slovakia based on magnetotelluric sounding of deep tectonic structures

Autorzy:

Bezák, Vladimír
Vozár, Ján
Majcin, Dušan
Klanica, Radek
Madarás, Ján

Powiązania:

https://bibliotekanauki.pl/articles/2059582.pdf

Data publikacji:

2021

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Western Carpathians
Klippen Belt
magnetotelluric sounding
subduction
collision
transpression

Opis:

To characterize the deep structure of the Klippen Belt, we made magnetotelluric measurements in profiles across the western and eastern segments in the territory of Slovakia, from which we created 3D models. The models revealed significant differences in tectonic structure between these segments. In the western segment, the Klippen Belt is located in the southern reversing wing of the original subduction flower structure (retroarc thrusting) with an overthrust to the south onto the Inner Western Carpathian units. This structure was later modified by significant transpressional movements. In the eastern segment, the Klippen Belt is primarily an organic part of the accretionary wedge of the Outer Western Carpathians and it is overthrusted onto the Flysch Belt. This was followed by modification of the structures, mostly in a transpressional regime, including local reversing overthrusts and the development of a steep fault boundary, mainly along the southern margin, against the Inner Carpathian Paleogene succession. These differences between the structure of the western and eastern Klippen Belt segments indicate the contrast between the interaction of the western and eastern parts of the Inner Western Carpathians with the European Platform. In the western part, oblique collision and sinistral transpression dominate. In the eastern part, by contrast, subduction and orthogonal collision dominated over later transpressional modifications.

Źródło:

Geological Quarterly; 2021, 65, 2; 65: 25
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 19.

Tytuł:

Piping in loess-like and loess-derived soils : case study of Halenkovice site, Czech Republic

Autorzy:

Bíl, M.
Kubeček, J.

Powiązania:

https://bibliotekanauki.pl/articles/191487.pdf

Data publikacji:

2012

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

soil piping
subsurface flow
Outer Western Carpathians
Czech Republic

Opis:

The soil piping that occurs on luvisols in the vicinity of the village of Halenkovice was studied for 5 years. These piping phenomena can only be found where arable land meets the forest or a belt of shrubbery. If there is a scarp in the locality, which usually changes from 6° in the field to approximately 30° in the forest, soil pipes are more likely to occur. Before the scarp, the slope flattens out and it is almost horizontal. This factor makes it possible for the overland flow to seep into the slope. This seepage results in soil piping, which is formed in loess loam and colluvial deposits. There are about 15 sites in the vicinity of the village of Halenkovice, where soil piping occurs. In one of them, Halenkovice 1 (an area of 900 m2) we closely studied 47 partial cavities. Their internal volume is 3.8 m3. The volume of the sink holes is 23 m3. There are two types of soil pipes – vertical, which on average tend to be shorter (40 cm) and lead the water under the surface, and soil pipes parallel with the slope, which are on average 81 cm long. Water flows through the pipes during a thaw or precipitation, which often takes away the top soil. The intensity of this process depends on the intensity of precipitation, which occurs outside the growing season, when there are no crops in the fields.

Źródło:

Annales Societatis Geologorum Poloniae; 2012, 82, 1; 45--50
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 20.

Tytuł:

Tectonic control of cave developmen t: a case study of the Bystra Valley in the Tatra Mts., Poland

Autorzy:

Szczygieł, J.
Gaidzik, K.
Kicińska, D.

Powiązania:

https://bibliotekanauki.pl/articles/191732.pdf

Data publikacji:

2015

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

Cave morphology
speleogenesis
tectonics
neotectonics
Tatra Mts.
Western Carpathians

Opis:

Tectonic research and morphological observations were carried out in six caves (Kalacka, Goryczkowa, Kasprowa Niżna, Kasprowa Średnia, Kasprowa Wyżnia and Magurska) in the Bystra Valley, in the Tatra Mountains. There are three cave levels, with the youngest active and the other two inactive, reflecting development partly under epiphreatic and partly under phreatic conditions. These studies demonstrate strong control of the cave pattern by tectonic features, including faults and related fractures that originated or were rejuvenated during uplift, lasting from the Late Miocene. In a few local cases, the cave passages are guided by the combined influence of bedding, joints and fractures in the hinge zone of a chevron anticline. That these cave passages are guided by tectonic structures, irrespective of lithological differences, indicates that these proto-conduits were formed by “tectonic inception”. Differences in the cave pattern between the phreatic and epiphreatic zones at a given cave level may be a result of massif relaxation. Below the bottom of the valley, the effect of stress on the rock mass is related to the regional stress field and only individual faults extend below the bottom of the valley. Thus in the phreatic zone, the flow is focused and a single conduit becomes enlarged. The local extension is more intense in the epiphreatic zone above the valley floor and more fractures have been sufficiently extended to allow water to flow. The water migrates along a network of fissures and a maze could be forming. Neotectonic displacements (of up to 15 cm), which are more recent than the passages, were also identified in the caves. Neotectonic activity is no longer believed to have as great an impact on cave morphology as previously was thought. Those faults with displacements of several metres, described as younger than the cave by other authors, should be reclassified as older faults, the surfaces of which have been exposed by speleogenesis. The possible presence of neotectonic faults with greater displacements is not excluded, but they would have had a much greater morphological impact than the observed features suggest.

Źródło:

Annales Societatis Geologorum Poloniae; 2015, 85, 2; 387-404
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 21.

Tytuł:

Bronzezeitliches Siedlungswesen im Vorfeld der polnischen Westkarpaten: Geomagnetische Untersuchungen und Geländebegehungen im Bereich des Dunajectals
The specificity of the Bronze Age settlement in the foreland of Polish Western Carpathians. Surface surveys and geomagnetic prospection in the valley of the Dunajec River

Autorzy:

Kienlin, Tobias L.
Valde-Nowak, Paweł

Powiązania:

https://bibliotekanauki.pl/articles/442426.pdf

Data publikacji:

2009

Wydawca:

Uniwersytet Jagielloński. Instytut Archeologii

Tematy:

Polish Western Carpathians
Bronze Age
surface surveys
geomagnetic prospection

Opis:

In 2006, the verification surface surveys and geomagnetic prospection were carried out on Neolithic and Bronze Age sites in Wiśnicz and Rożnów Foothills. These sites were discovered in the course of AZP action in the early 90s the last century. The research were undertaken in order to obtain further information on the source potential and character of the settlement. For geomagnetic prospection 15 sites were selected. As a result of the research it was possible to significantly increase the amount of the Early and Older Bronze Age, which are fairly rare in the Carpathians. Particular attention was paid to extensive field scatterings of pottery dated at later periods of the Bronze Age and probably also at the Iron Age. In several sites, as can be judged on the results of geomagnetic prospections, there are numerous features embedded in the ground. In that case, a systematic excavation should be carried out. Of these sites a big highland settlement in Janowice seems to be the most spectacular.

Źródło:

Recherches Archéologiques Nouvelle Serie; 2009, 1; 49-71
0137-3285

Pojawia się w:

Recherches Archéologiques Nouvelle Serie

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 22.

Tytuł:

Stepwise clockwise rotation of the Cenozoic stress field in the Western Carpathians as revealed by kinematic analysis of minor faults in the Manín Unit (western Slovakia)

Autorzy:

Šimonová, V.
Plašienka, D.

Powiązania:

https://bibliotekanauki.pl/articles/2060350.pdf

Data publikacji:

2017

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

faults
palaeostress reconstruction
tectonic regime
Manín Unit
Western Carpathians

Opis:

This study aims at quantitative kinematic analysis of fault-slip data and palaeostress reconstruction of polyphase brittle structures developed in the Manín Unit cropping out in the Middle Váh River Valley of western Slovakia. The Manín Unit neighbours the Pieniny Klippen Belt that follows the boundary between the Paleogene accretionary wedge of the Outer Carpathians and the Cretaceous nappe system of the Central Western Carpathians. After the nappe emplacement during mid-Cretaceous times, the Manín Unit was incorporated into the Pieniny Klippen Belt and attained its complex tectonic style. Based on kinematic analysis of meso-scale faults with slickensides, six (D1–D6) brittle deformation stages have been discerned. The relative succession of individual palaeostress states was derived from field structural relationships; their stratigraphic age was estimated primarily by comparison with other published data. Palaeostress analysis in the Manín Unit revealed the existence of six different palaeostress fields acting from the Middle Eocene to the Quaternary. The first three generations of meso-scale brittle structures were formed under a transpressional tectonic regime during the pre-Late Eocene–Early Miocene D1–D3 deformation. Generally, the maximum horizontal stress axis rotated clockwise from a W–E to an approximately N–S direction. Thereafter, a transtensional tectonic regime was characterized by a WNW–ESE to NNW–SSE oriented minimum horizontal stress axis during Middle and Late Miocene D4–D5 deformation. A general extensional tectonic regime influenced the structural evolution of the area in the Pliocene to Quaternary, when a gradual reorientation of the palaeostress field resulted in the development of variable, often reactivated, fault structures.

Źródło:

Geological Quarterly; 2017, 61, 1; 251--264
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 23.

Tytuł:

Chromian spinels from the Magura Unit (Western Carpathians, Eastern Slovakia) : their petrogenetic and palaeogeographic implications

Autorzy:

Bónová, K.
Špisiak, J.
Bóna, J.
Kováčik, M.

Powiązania:

https://bibliotekanauki.pl/articles/2060358.pdf

Data publikacji:

2017

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Western Carpathians
Magura Basin
provenance
detrital chromian spinel
geochemistry

Opis:

Detrital chromian spinels in sedimentary rocks provide much information concerning the tectonics of their parental ultrabasic rocks. Chromian spinels occurring in the Eocene to Oligocene depos its from the Magura Nappe were exam i ned to provide some constraints on the history of the Magura Basin. The Magura Nappe is a part of the Flysch Belt belonging to the External Western Carpathians. The Magura Nappe is separated by a narrow zone associated with the Pieniny Klippen Belt and is divided into three principal tectono-lithofacies units (from the S to N): the Krynica, Bystrica and Rača units. Cr-spinel is a common accessory mineral (2.3-5.9 vol% of heavy mineral spectra) in the siliciclastic rocks of the Rača and Krynica units. In terms of texture and chemical composition, two types of Cr-spinels were recognized: unaltered and altered. Unaltered spinels were found to contain silicate inclusions such as chromio-pargasite, enstatite, diopside, pargasite, plagioclase and olivine (forsterite). The chromian spinels show wide variations in compositional parameters such as Cr# (0.3-0.7), Mg# (0.3-0.7), TiO2 (<0.03-1.9 wt.%) and Fe2+/Fe3+ (2.5-13) whereas the differences between the Rača and Krynica units are in- significant. These parameters suggest a peridotitic and volcanic origin of the spinels, respectively. The ophiolite source consisting of harzburgitic mantle peridotites was developed mainly in a supra-subduction zone setting; volcanic spinels indicate an origin in mid-ocean ridge basalts, back-arc basin basalts and sporadically in ocean-island basalts. Concerning their geochem i cal features, we propose that during the Eocene to Early Oligocene, the ophiolitic detritus in the eastern part of the Magura Basin deposits may have been derived from a source area located in the Fore-Marmarosh Suture Zone (Eastern Carpathians) that is considered an equivalent of the Black Flysch and Ceahlau units. Some Cr-spinels found in the Eocene sedimentary successions may have resedimented from older Late Cretaceous-Paleocene formations of the Magura Unit, which are considered as reworked sedimentary material from the Pieniny Klippen Belt.

Źródło:

Geological Quarterly; 2017, 61, 1; 3--18
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 24.

Tytuł:

A multicriteria approach to different land use scenarios in the Western Carpathians with the SWAT model

Autorzy:

Kowalczyk, Agnieszka W.
Grabowska-Polanowska, Beata
Garbowski, Tomasz
Kopacz, Marek
Lach, Stanisław
Mazur, Robert

Powiązania:

https://bibliotekanauki.pl/articles/27312653.pdf

Data publikacji:

2023

Wydawca:

Instytut Technologiczno-Przyrodniczy

Tematy:

catchment area
land use
soil erosion
SWAT model
Western Carpathians

Opis:

Water erosion in mountainous areas is a major problem, especially on steep slopes exposed to intense precipitation. This paper presents the analysis of the topsoil loss using the SWAT (Soil and Water Assessment Tool) model. The SWAT model is a deterministic catchment model with a daily time step. It was designed to anticipate changes taking place in the catchment area, such as climate change and changes in land use and development, including the quantity and quality of water resources, soil erosion and agricultural production. In addition to hydrological and environmental aspects, the SWAT model is used to address socio-economic and demographic issues, such as water supply and food production. This program is integrated with QGIS software. The results were evaluated using the following statistical coefficients: determination (R2), Nash-Sutcliff model efficiency (NS), and percentage deviation index (PBIAS). An assessment of modelling results was made in terms of their variation according to different land cover scenarios. In the case of the scenario with no change in use, the average annual loss of topsoil (average upland sediment yield) was found to be 14.3 Mg∙ha-1. The maximum upland sediment yield was 94.6 Mg∙ha-1. On the other hand, there is an accumulation of soil material in the lower part of the catchment (in-stream sediment change), on average 13.27 Mg∙ha-1 per year.

Źródło:

Journal of Water and Land Development; 2023, 57; 130--139
1429-7426
2083-4535

Pojawia się w:

Journal of Water and Land Development

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 25.

Tytuł:

„Depositional setting of the Oligocene sequence of the Western Carpathians in the Polish Spisz region : a reinterpretation based on integrated palynofacies and sedimentological analyses” – Discussion

Autorzy:

Gedl, P.

Powiązania:

https://bibliotekanauki.pl/articles/2060423.pdf

Data publikacji:

2018

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Oligocene sequence
Western Carpathians
Polish Spisz region
palynofacies
sedimentological analyses

Opis:

In their recent paper, Filipek et al. (2017) provided some data on age (dinoflagellate cyst biostratigraphy) and sedimentary setting (sedimentological and palynofacial analysis) of the Podhale Flysch (Central Carpathian Paleogene) from the Polish Spisz (their fig. 1). They carried out their integrated studies on the middle part of the Podhale Flysch succession – the upper part of the Szaflary beds through the lower part of the Chochołów beds. These studies, as stated in Introduction, “…allow for a new approach to the knowledge on the CCPB with regard to stratigraphy, depositional palaeoenvironment, and changes during deposition”.

Źródło:

Geological Quarterly; 2018, 62, 3; 745--750
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 26.

Tytuł:

Tectonic control of tufa occurrences in the Podhale Synclinorium (Central Western Carpathians, southern Poland)

Autorzy:

Mastella, L.
Rybak-Ostrowska, B.

Powiązania:

https://bibliotekanauki.pl/articles/2060528.pdf

Data publikacji:

2012

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

tufas
fault zones
active tectonics
Podhale Synclinorium
Central Western Carpathians

Opis:

Tufas in the Podhale Synclinorium (southern Poland) occur as encrustations on moss and plant remains, crusts, porous, clastic and massive tufas. The tufas are almost entirely composed of calcite with small admixture of quartz, illite and chlorite. These deposits indicate the biotic and/or abiotic origin of calcium carbonate. The tufas occur in the vicinity of map-scale and minor fault zones. They precipitate near fissure springs linked with small faults and fault rocks or seepages along them. Exposures with tufas occur along several oblique and lateral zones. The oblique zones are related to Białka and Biały Dunajec faults that have normal components. The lateral zones of tufa occurrences are connected with lateral faults limiting the “zone of beds with gentle dips” and extensional brittle structures within the hinge of the synclinorium. The relationship of the tufa with brittle extensional structures suggests Quaternary tectonic activity of the Podhale Synclinorium that can be explained by continued uplift in the area studied.

Źródło:

Geological Quarterly; 2012, 56, 4; 733--744
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 27.

Tytuł:

Trace element geochemistry of the Early to Late Cretaceous deposits of the Grajcarek thrust-sheets - a palaeoenvironmental approach (Małe Pieniny Mts., Pieniny Klippen Belt, Poland)

Autorzy:

Wójcik-Tabol, P.
Oszczypko, N.

Powiązania:

https://bibliotekanauki.pl/articles/2058965.pdf

Data publikacji:

2012

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Western Carpathians
Grajcarek thrust-sheets
black flysch
trace elements geochemistry

Opis:

The chemical composition of the Cretaceous deposits of the Grajcarek thrust-sheets (Pieniny Klippen Belt, Poland) has been investigated to provide information on palaeoenvironment and provenance of pelagic and turbiditic particles. The material studied shows large variations in terrigenous and biogenic content. Phyllosilicates (mirrored in amounts of Al2O3, average 15 wt.%) and carbonates (6 wt.% of CaO) are common mineral components of the deposits excluding the Cenomanian radiolarian shales (CRS) that are enriched in silica "Immobile" elements may be accommodated by phyllosilicates and accessory minerals (i.e. zircon, xenotime, apatite and Ti-oxides). Heavy minerals are significant within the Szlachtowa Fm. High field strength elements (HFSE) in the Malinowa Fm. are housed in secondary apatite and Fe-oxides. Lithophile trace elements (LILE) concentrations in the material studied are lower/comparable to Post-Archean Australian Shale (PAAS). Ba concentration in the CRS probably reflects enhanced bioproductivity. Interaction between major oxides, distributions of "immobile' and lithophile elements suggest that variation in trace elements through the succession was mainly controlled by the terrigenous input. The material studied was sourced from intermediate to felsic rocks of the Czorsztyn (Oravic) Ridge. The Szlachtowa Fm. and CRS are more mature than others due to low contents of clay minerals. The Szlachtowa Fm. also contains recycled material. The CRS correspond to the oceanic anoxic event 2 (OAE 2) whereas the "Black Flysch" of the Szlachtowa and Opaleniec formations may be related to the Early Cretaceous OAE 1

Źródło:

Geological Quarterly; 2012, 56, 1; 169-186
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 28.

Tytuł:

Oligocene-Lower Miocene sequences of the Pieniny Klippen Belt and adjacent Magura Nappe between Jarabina and the Poprad River (East Slovakia and South Poland): their tectonic position and palaeogeographic implications

Autorzy:

Oszczypko, N.
Oszczypko-Clowes, M.
Golonka, J.
Marko, F.

Powiązania:

https://bibliotekanauki.pl/articles/2059696.pdf

Data publikacji:

2005

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Outer Western Carpathians
Pieniny Klippen Belt
lithostratigraphy
biostratigraphy
suture zone

Opis:

This paper provides the results of a new litho- and biostratigraphic study from the contact zone between the Magura Nappe and Pieniny Klippen Belt close to Polish-Slovakian border. In the southernmost part of the Krynica facies zone of the Magura Nappe two new lithostratigraphic units have been established: the Poprad Member and the Kremna Formation. The Late Eocene-Oligocene age of the Malcov Formation (NP 19-NP 24) of the Pieniny Klippen Belt has also been confirmed. A Late Oligocene age (Zone NP 25 and lower part of NN1) was determined in deposits belonging to the Poprad Member of theMagura Formation, while an EarlyMiocene age (upper part of NN1 and NN2 zones) was established for the Kremna Formation. The Late Cretaceous-MiddleMiocene geotectonic evolution of the orogenic suture zone, between the Inner and Outer Carpathians, is outlined.

Źródło:

Geological Quarterly; 2005, 49, 4; 379--402
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 29.

Tytuł:

Solution-collapse breccias in the upper Olenekian–Ladinian succession, Tatra Mts, Poland

Autorzy:

Jaglarz, P.
Rychliński, T.

Powiązania:

https://bibliotekanauki.pl/articles/191208.pdf

Data publikacji:

2018

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

palaeokarst
evaporites
solution breccia
dolomitization
diagenesis
Tatricum
Triassic
Western Carpathians

Opis:

The upper Olenekian-Middle Triassic succession of the Tatricum domain (Central Western Carpathians, southern Poland) includes a few horizons of breccias, which are intercalated with early-diagenetic dolostones. On the basis of macroscopic and microscopic (including cathodoluminescence) observations, the paper presents a new interpretation of the genesis of the breccias and their diagenetic history. The rocks studied range from monomictic, cemented mosaic packbreccias to chaotic, unsorted, monomictic, particulate rubble floatbreccias. The processes that preceded the formation of the breccias encompassed the precipitation of evaporites and the early-diagenetic dolomitization of lime muds. The solution-collapse breccias were formed during episodes of cyclic sediment emersions in the upper Olenekian and Middle Triassic, as the result of gradual sediment collapse after karstic dissolution of the intercalated evaporites. After the brecciation process, during diagenesis the rocks were subjected to cementation by sulphate minerals and next, to multi-stage dolomitization. Later tectonic processes led to fracturing and even re-brecciation of the previously formed solution-collapse breccias.

Źródło:

Annales Societatis Geologorum Poloniae; 2018, 88, 4; 303-319
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 30.

Tytuł:

Microfabric diversity and grain shape analysis of fault rocks from the selected areas of the Western Tatra Mountains

Autorzy:

Kania, M.

Powiązania:

https://bibliotekanauki.pl/articles/2059963.pdf

Data publikacji:

2014

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

microfabrics
grain shape analysis
fault rocks
shear zones
Western Carpathians
Western Tatra Mountains

Opis:

Fault rocks in brittle and brittle-ductile shear zones played a key role in the evolution of the Western Tatra Mountains crystal- line rocks (Poland-Slovakia). Microfabrics of these rocks, including grain shape analyses, were investigated in the six areas of the Western Tatra Mountains. Based on studies of thin sections, 14 types of fault rock microfabric are distinguished, ac- cording to the following criteria: (a) the presence and abundance levels of a cataclastic matrix and (b) the presence and form of a preferred orientation features. General tendencies observed in these areas indicate southwards increasing non-coaxial deformation as well as the domination of ultracataclasites or ultramylonites to phyllonites in areas with negative relief (e.g., sedlo Zabrat’ Pass, Dziurawa Przełęcz Pass). A model of shear zone evo l u tion embracl ng foll owl ng three stages is pro- posed: (1) deformation partitioning and block-controlled cataclastic flow, (2) matrix-controlled cataclastic flow, (3) selective leaching and deposition of silica, leading to the formation of softened and hardened deformation domains respectively. These microstructural observations were supported by statistical analyses of the grain shape indicators (compactness, isometry, ellipticity, solidity, convexity). Two trends of relationships between compactness and convexity were noted: the first, horizontal on the correlation diagrams, was interpreted as an effect of rapid cataclasis and then sericitization, the sec- ond, with a strongly negative correlation coefficient, was considered as an effect of long-term cataclastic flow. The different microfabric data and microstructural interpretations described in this paper are consistent with a new model of the tectonic history of the Western Tatra Mountains evolution, with an important role for a non-coaxial deformation during Alpine orogeny in brittle and brittle-ductile conditions.

Źródło:

Geological Quarterly; 2014, 58, 1; 3--18
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 31.

Tytuł:

“Late Hallstatt” hillforts in the Western Carpathians: new contribution to an old discussion

Autorzy:

Danielová, Barbora Lofajová
Markiewicz, Joanna A.
Przybyła, Marcin S.
Ledwoń, Jan

Powiązania:

https://bibliotekanauki.pl/articles/2041008.pdf

Data publikacji:

2021

Wydawca:

Uniwersytet Jagielloński. Wydawnictwo Uniwersytetu Jagiellońskiego

Tematy:

Early Iron Age
La Tène period
Western Carpathians
hillforts
prehistoric fortifications

Opis:

The article presents new research on fortified settlements from the Early Iron Age in the Orava and Dunajec river valleys. Based on the characteristics of the construction of the fortifications and similarities in terms of material culture, we propose recognizing the hillforts discovered here as a manifestation of one cultural and settlement horizon related to the so-called Pre-Púchov stage. The radiocarbon determinations obtained for the contexts stratigraphically related to the ramparts from the Nižná-Ostražica, Zabrzeż-Babia Góra, and Maszkowice-Góra Zyndrama sites are already located on the calibration curve after the so-called Hallstatt plateau and allow this horizon to be dated to the 4th century BC, i.e. to the times corresponding to the La Tène B1–B2 phases. Our observations confirm the opinions appearing in more recent literature about the need to date the Pre-Púchov stage in Slovakia earlier, and discuss the thesis about the continuation of settlement at the beginning of the La Tène period. With regard to the Polish Carpathian zone, arguments indicating the possibility of the survival of settlements with Early Iron Age traditions up to the 4th century BC are presented for the first time. This allows us to assume that the process of the formation of the cultural tradition of the La Tène period here progressed in a similar manner to Slovakia, and it was not solely the result of migration from the latter.

Źródło:

Acta Archaeologica Carpathica; 2021, 56; 221-256
0001-5229
2719-4841

Pojawia się w:

Acta Archaeologica Carpathica

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 32.

Tytuł:

Heavy minerals from sedimentary rocks of the Malcov Formation and their palaeogeographic implications for evolution of the Magura Basin (Western Carpathians, Slovakia) during the Late Eocene–Late Oligocene

Autorzy:

Bónová, K.
Bóna, J.
Kováčik, M.
Laurinc, D.

Powiązania:

https://bibliotekanauki.pl/articles/2059937.pdf

Data publikacji:

2016

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Western Carpathians
Magura Nappe
Malcov Formation
provenance
heavy minerals
mineral composition

Opis:

Detrital heavy minerals separated from the Malcov Fm. deposits (Magura Nappe) indicate their source rocks and areas. The heavy mineral assemblages predominantly consist of garnet, zircon, tourmaline, rutile and Cr-spinel. EPMA analyses reveal a few groups of garnets: zoned and unzoned Grs almandines, Prp-Sps almandines, unzoned Prp almandines, almandines, Sps almandines and rare zoned spessartine grains (~85 mol% Sps). The garnet composition indicates that gneisses, mica schists, amphibolites and granites were their main source rocks, but low-grade metapelites with Mn mineralisation probably contributed as well. The detrital dravitic tourmalines were mostly derived from paragneisses and mica schists. Cr-spinel indicates a volcanic source. Based on heavy mineral assemblages, coupled with palaeoflow analysis, we conclude that the Marmarosh Massif and Fore-Marmarosh Suture are the most probable source areas. Aditionally, the Malcov sedimentary basin was supplied by material from the crystalline complexes of the Tisza Mega-Unit and Pieniny Klippen Belt (PKB). The bulk of the clastic deposits comprise classical turbidites. These lithofacies were deposited from either turbidity currents or from concentrated density flows. The palaeoflow record is varied and highlights the contribution of sedimentary material from several directions and/or diversion of gravity currents from the main flow direction (SE–NW). The marginal parts of the Malcov sub-basins were formed of deformed and uplifted older formations of surrounding units of the Magura Nappe and PKB (submerged ridges). Older (Late Cretaceous to Eocene) flysch sediments may have been redeposited from these ridges to neighbouring sub-basins in a transverse direction (NE–SW).

Źródło:

Geological Quarterly; 2016, 60, 3; 675--694
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 33.

Tytuł:

Sole structures as a tool for depositional environment interpretation : a case study from the Oligocene Cergowa Sandstone, Dukla Unit (Outer Carpathians, Slovakia)

Autorzy:

Dirnerová, D.
Janočko, J.

Powiązania:

https://bibliotekanauki.pl/articles/2059973.pdf

Data publikacji:

2014

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

sedimentology
sole structures
flow properties
Dukla Unit
Cergowa sandstone
Western Carpathians

Opis:

Sole structures, typically developed on basal bedding surfaces of turbidite sandstones, are commonly used as palaeocurrent indicators and indicators of the current ability to erode. Detailed analysis of types and frequency of sole structures in the 128 m thick succession of Early Oligocene Cergowa Sandstone (Outer Western Carpathians) also shows their potential as an indicator of flow condition during the deposition. The massive and amalgamated sandstones, predominantly containing load casts and minor flutes and grooves with unidirectional orientation, are suggested to be deposited by highly turbulent flow after reaching hydraulic jump behind the topographic obstacle. High range of sole structures in thick and medium thick sandstones, suggesting inferior oblique and reverse flows, implies deposition from density stratified flows where lower, denser part has a tendency to deflect when hit the basin floor obstacle. The upper, less dense part has an ability to come over the obstacle and shows only small scatter in the palaeocurrent direction.

Źródło:

Geological Quarterly; 2014, 58, 1; 41--50
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 34.

Tytuł:

Pliocene to Quaternary stress field change in the western part of the Cen tral West ern Carpathians (Slovakia)

Autorzy:

Vojtko, R.
Hók, J.
Kováč, M.
Sliva, L’.
Joniak, P.
Šujan, M.

Powiązania:

https://bibliotekanauki.pl/articles/2060207.pdf

Data publikacji:

2008

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Western Carpathians
fault-slip data
Quaternary stress field
neotectonics
palaeostress analysis

Opis:

Knowledge of the current tectonic regime plays an essential role in natural hazard assessment, especially in the risk assessment of fault activity. Structural analysis of brittle deformations (using in version techniques) was used to determine the stress field state occurring within Pliocene and Quaternary deposits in the western part of the Central Western Carpathians. The deformation pattern of the reduced stress tensor showed that all structural measurements could be separated into two groups. An older, Late Pliocene fault population was activated un der NNW-SSE oriented extension. A younger, Quaternary fault population reflected origin in a NE–SW extensional tectonic regime and it distinctly showed a change the orientation of the S3 of about 70. The change in tectonic activity, as well as in the stress field orientation, is dated to the Pliocene-Pleis to cene boundary. The Quaternary stress field developed dur ing the post-collisional stage of the orogen. Our study shows that the West ern Carpathian internal units document NE-SW to NNE-SSW extension in the broader region around of the north ern Danube Basin.

Źródło:

Geological Quarterly; 2008, 52, 1; 19-19
1641-7291

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Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 35.

Tytuł:

Needle-fibre calcite and nanofibres as components of Holocene fissure-filling carbonates in southern Poland

Autorzy:

Gradziński, M.
Jach, R.
Górnikiewcz, R.

Powiązania:

https://bibliotekanauki.pl/articles/191986.pdf

Data publikacji:

2013

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

speleothems
caliche
stable isotopes
radiocarbon dating
Pieniny Klippen Belt
Western Carpathians

Opis:

The article deals with the carbonates, filling fissures in limestone bedrock and presently exposed in a south-facing rock wall of Kramnica hill (Pieniny Klippen Belt, southern Poland). The carbonates are composed of (i) needle-fibre calcite crystals, (ii) carbonate nanofibres, (iii) carbonate nanoparticles, and (iv) micrite and sparite calcite crystals. Detrital grains from the carbonate bedrock occur subordinately. The spatial relationships of the components give documentation that the nanofibres were formed simultaneously with or slightly later than the needle-fibre calcite crystals. There exists a continuous chain of forms from nanoparticles to elongated nanofibres. This, in turn, indicates that all the above morphological forms are related genetically. In relatively wide fissures, the carbonates studied formed stepped microterracettes, similar to those of speleothems, mainly of moonmilk type. Conversely, narrow fissures are completely filled with carbonates, which display parallel lamination. The carbonates were formed in the late Holocene. However, “dead carbon effect” precludes the possibility of any precise dating of them. Their δ13C and δ18O values are in ranges from -5.1‰ to -3.8‰ and from -6‰ to -4.7‰, respectively. The carbonates studied bear a strong resemblance to soil and spelean, moonmilk-type carbonates. This indicates that continuity exists between the depositional environments of soil and spelean carbonate.

Źródło:

Annales Societatis Geologorum Poloniae; 2013, 83, 3; 229-242
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 36.

Tytuł:

Stratigraphy and palaeo- geographic position of the Jurassic Czertezik Succession, Pieniny Klippen Belt (Western Carpathians) of Poland and Eastern Slovakia

Autorzy:

Wierzbowski, A.
Aubrecht, R.
Krobicki, M.
Matyja, B. A.
Schlögl, J.

Powiązania:

https://bibliotekanauki.pl/articles/191597.pdf

Data publikacji:

2004

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

Jurassic
Western Carpathians
Pieniny Klippen Belt
Czertezik Succession
stratigraphy
ammonites
palaeogeography

Opis:

The Czertezik Succession has been closely re-examined in its most classical sections of the Pieniny Klippen Belt (Western Carpathians) in Poland and eastern Slovakia. The study revealed the presence of the "lower nodular limestones" (Niedzica Limestone Formation), and resulted in discovery of Early Bajocian ammonite fauna in grey crinoidal limestones of the Smolegowa Limestone Formation/Flaki Limestone Formation, and the latest Bajocian to Early Bathonian ammonite fauna in the Niedzica Limestone Formation. These new data proved closer similarity between the Czertezik Succession and the Niedzica Succession than between the Czertezik Succession and the Czorsztyn Succession as it was suggested up to now. On the other hand, the Czertezik Succession represents deeper palaeogeographical position within the Pieniny Klippen Basin than the Niedzica Succession and it has been deposited near the Branisko/Kysuca Succession.

Źródło:

Annales Societatis Geologorum Poloniae; 2004, 74, No 3; 237-256
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 37.

Tytuł:

Geotourism valorisation of selected quarries of kłodzko region and cieszyn foothills

Autorzy:

Kasprowska-Nowak, Katarzyna
Marek, Aneta

Powiązania:

https://bibliotekanauki.pl/articles/1051068.pdf

Data publikacji:

2019-03-31

Wydawca:

Uniwersytet im. Adama Mickiewicza w Poznaniu

Tematy:

Eastern and Central Sudetes
Outer Western Carpathians
quarries
valorisation criteria
geotourism

Opis:

The article presents a geotourism valorisation of selected quarries located in different mountainous regions in southern Poland, diverse in geological and tectonic terms. The regions of Kłodzko (with quarries Kletno I, Krzyżnik, Sinica, Czarne Urwisko, Szczytna Zamek) and of Cieszyn Foothills (quarries Na Jasieniowej, Na Mołczynie, Grota na Rudowie, Nad Kalembianką, Ondraszkowa Dziura) were proposed as a case study. The survey describes the most exposed disused quarries of marble, gneiss, sandstone, teschenites and Cieszyn limestone of high natural and cultural significance. As a result of the geotourist valorisation, the analysed geological objects were given point score under various criteria (educational value, scientific value, visual value, location/accessibility value, cultural value, geo-infrastructural value and the value of legal protection). It was found that the discussed quarries reveal high natural and educational value, and they are very significant in education and promotion of geologically attractive areas.

Źródło:

Quaestiones Geographicae; 2019, 38, 1; 41-51
0137-477X
2081-6383

Pojawia się w:

Quaestiones Geographicae

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 38.

Tytuł:

Radiocarbon dating of fossil bats from Dobšina Ice Cave (Slovakia) and potential palaeoclimatic implications

Autorzy:

Gradziński, M.
Hercman, H.
Peresviet-Soltan, A.
Zelinka, J.
Jelonek, M.

Powiązania:

https://bibliotekanauki.pl/articles/973695.pdf

Data publikacji:

2016

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

Little Ice Age
Medieval Warm Period
perennial cave ice
Western Carpathians

Opis:

Although Dobšina Ice Cave (DIC, Carpathians, Slovakia) is located outside the high-mountain area, it hosts one of the most extensive blocks of perennial subterranean ice, the volume of which is estimated at more than 110,000 m3. Frozen bat remains were found in the lowermost part of the perennial ice block. They belong to Myotis blythii (Tomes) and the M. mystacinus morpho-group. The radiocarbon dating of bat soft tissues yielded ages of 1266–1074 cal. yr BP and 1173–969 cal. yr BP. The undetermined bat, found in the same part of the ice section in 2002, was previously dated at 1178–988 cal. yr BP (Clausen et al., 2007). The dates testify that the ice crystallized at the turn of the Dark Ages Cold Period and the Medieval Warm Period. The calculated accumulation rate of cave ice varies between 0.7 cm/year and 1.4 cm/year at that time, and is similar to the present ice accumulation rate in DIC. Constant crystallization of ice during the Medieval Warm Period is hypothesized to reflect dry summer seasons since the supply of relatively warm water in the summer is one of the key factors causing the erosion of cave ice. The uppermost sample was covered with 20.6 m of ice. Between ca 1065 cal. yr BP and the present day, the ice grew faster than between ca 1210 yr BP and ca 1065 yr BP by a factor of 1.3–1.8. This may have resulted from conditions favourable for ice accumulation during the Little Ice Age.

Źródło:

Annales Societatis Geologorum Poloniae; 2016, 86, 3; 341-350
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 39.

Tytuł:

Jurassic syn-rift and Cretaceous syn-orogenic, coarse-grained deposits related to opening and closure of the Vahic (South Penninic) Ocean in the Western Carpathians – an overview

Autorzy:

Plasienka, D.

Powiązania:

https://bibliotekanauki.pl/articles/2060512.pdf

Data publikacji:

2012

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Western Carpathians
Mesozoic
rifting
thrusting
deep-marine clastics
mass flow deposits

Opis:

Although no undoubted oceanic crustal rock complexes of Penninic affinity participate in the present surface structure of the Western Carpathians, indirect lines of evidence suggest prolongation of the South Penninic-Vahic oceanic tract into the ancient Carpathians. The sedimentary record of both the syn-rift and syn-orogenic clastic deposits reveal their origin between the outer Tatric (Austroalpine) and the inner Oravic (Middle Penninic) margins. The rifting regime is exemplified by the normal fault-related scarp breccias of the Jurassic Borinka Unit in the Male Karpaty Mts., which are characterized by local, gradually denuded source areas. Two other regions provide examples of a contractional regime, both related to shortening and closure of the Vahic oceanic domain. The Belice Unit in the Povazsky Inovec Mts. includes Upper Jurassic-Lower Cretaceous eupelagic, mostly siliceous deposits and a thickening-upwards Senonian sequence of turbiditic sandstones, conglomerates and chaotic breccias. It is inferred that this succession represents the sedimentary cover of oceanic crust approaching a trench, its incorporation in the accretionary complex and finally underthrusting below the outer Tatric margin. In the Oravic units of the Pieniny Klippen Belt, deep-marine conglomerate/breccia bodies with olistoliths indicate collision-related thrust stacking that started from the Maastrichtian (Gregorianka Breccia of the Sub-Pieniny Unit) and terminated with the Lower Eocene Milpos Breccia in the Saris Unit. In addition, a tentative recycling scheme of “exotic” clastic material from mid-Cretaceous conglomerates of the Klape Unit to various Klippen Belt units is outlined. This material is considered to be unrelated to the Vahic oceanic realm and its closure, and likely represents erosional products of more distant orogenic zones.

Źródło:

Geological Quarterly; 2012, 56, 4; 601--628
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 40.

Tytuł:

Early and Middle Jurassic tectonically controlled deposition in the High-Tatric succession (Tatricum), Tatra Mountains, southern Poland : a review

Autorzy:

Łuczyński, Piotr

Powiązania:

https://bibliotekanauki.pl/articles/2058707.pdf

Data publikacji:

2021

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Central Western Carpathians
Vahic Ocean
Jurassic
High-Tatric series
synsedimentary tectonics

Opis:

The High-Tatric succession of the Tatra Mountains represents the Tatricum domain of the Central Western Carpathians, which in the Jurassic was located on the southern margin of the incipient and expanding Vahic Ocean – a branch of Western Tethys. This paper describes the various depositional consequences of extensional tectonic activity as it impacted on sedimentation in the High-Tatric succession of the Tatra Mountains during the Early and Middle Jurassic. Evidence of such impacts on depositional style and facies development are present within the Dudziniec, Smolegowa and Krupianka formations, in all the High-Tatric tectonic units. These impacts also include erosional surfaces and sedimentary gaps separating particular formations, commonly associated with minor angular unconformities. The Lower Jurassic, pre-Bajocian, Dudziniec Formation of the Kominy Tylkowe (autochthonous) Unit is developed in mixed carbonate-clastic facies. The occurrence and proportion of sand-dominated and carbonate-dominated facies, as well as their thickness differences, were controlled by syndepositional tilt-block tectonics, taking place both in depositional and in neighbouring source areas. The Smolegowa and Krupianka formations (Bajocian–Bathonian) occur in all High-Tatric tectonic units, but in the Czerwone Wierchy and Giewont units they are represented mainly by laterally discontinuous bodies of crinoidal limestone of very limited thickness. The preservation of these deposits only in some areas, as well as their thickness reductions, are effects of differentiated subsidence and uplift of isolated blocks taking place in an extensional regime. Moreover, the Krupianka Formation abounds in condensed facies with ferruginous crusts and stromatolites – a feature characteristic of rapidly drowning ocean margins. Deposits of the Dudziniec, Smolegowa and Krupianka formations are also preserved as infills of extensive systems of neptunian dykes penetrating mainly the Triassic substrate, which is yet another classic symptom of synsedimentary extension. The dominant influence of tectonics on sedimentary development ceased with the onset of deposition of the Raptawicka Turnia Formation in the Callovian.

Źródło:

Geological Quarterly; 2021, 65, 1; 16
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 41.

Tytuł:

Ruin marble : a record of fracture-controlled fluid flow and precipitation

Autorzy:

Marko, F.
Pivko, D.
Hurai, V.

Powiązania:

https://bibliotekanauki.pl/articles/2058871.pdf

Data publikacji:

2003

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Western Carpathians
fluids
healed joints
Liesegang rings
ruin marble
banded structures

Opis:

The ruin marble structure of the Cretaceous/Paleogene fine-grained marly limestone from the Outer Flysch Belt of the Western Carpathians has a non-tectonic origin, according to structural and sedimentological evidence. Distinctive offsets of coloured red-brownish ferric oxyhydroxide bands are not due to displacements along rock-cutting fractures, as they superficially appear to be. Evidences for shear movement along these pseudo-faults were not observed. Band offsets result from different velocities of pervasively diffusing fluids, precipitating ferric oxyhydroxides in corridors bounded by sets of mineralised systematic joints. During rock weathering, calcite-filled joints operated as barriers for lateral fluid diffusion, but enabled longitudinal diffusion along healed joints. Simple laboratory experiments have been performed to simulate the formation of natural ruin marble structure.

Źródło:

Geological Quarterly; 2003, 47, 3; 241-252
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 42.

Tytuł:

Pleistocene speleothem fracturing in the Western Carpathian orogenic foreland : A case study from transtensional setting at the eastern margin of the Bohemian Massif

Autorzy:

Babek, O.
Briestenský, M.
Přecechtělová, G.
Štěpančíková, P.
Hellstrom, J. C.
Drysdale, R. N.

Powiązania:

https://bibliotekanauki.pl/articles/2059654.pdf

Data publikacji:

2015

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

speleothems
U/Th series dating
palaeoseismicity
Pleistocene
Bohemian Massif
Western Carpathians

Opis:

We studied speleothem-fracturing styles and their tectonic context in three cave systems situated in the eastern Bohemian Massif, close to the Western Carpathians orogenic front: the Za hájovnou, Javoříčko, and Mladeč caves. The morphology of the speleothems in particularly thin stalactites, and supporting evidence from the cave interior, indicates a tectonic origin of the breakage. U/Th series dating of the stalactites, supported by Optically Stimulated Luminiscence (OSL) and 14C dating of soft sediments indicate that most of the fracturing occurred in the Upper Pleistocene, with the last fracturing events corresponding to MIS6 and MIS5 stages. OSL dating of faulted soft-sediment infill may even indicate that latest Pleistocene to Early Holocene tectonic events occurred in the Mladeč Cave. The speleothem fracturing is discussed in the regional context of the seismically active Nysa-Morava Zone situated at the junction between the Bohemian Massif (Elbe Fault Zone) and the Western Carpathians. This study provides the first evidence of palaeoseismicity from the subsurface and the oldest dated palaeoseismicity from the contact between the Western Carpathians and the Bohemian Massif.

Źródło:

Geological Quarterly; 2015, 59, 3; 491--506
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 43.

Tytuł:

New magnetic anomalies of the Outer Carpathians in NE Slovakia and their relationship to the Carpathian Conductivity Zone

Autorzy:

Kucharič, L.
Bezák, V.
Kubeš, P.
Konečný, V.
Vozár, J.

Powiązania:

https://bibliotekanauki.pl/articles/2060028.pdf

Data publikacji:

2013

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Western Carpathians
Flysch belt
Magnetic anomalies
Subvolcanic bodies
Carpathian Conductivity Anomaly

Opis:

A hitherto unknown magnetic anomaly has been detected in the framework of assembling magnetic picture of the Slovakian territory. The impressive magnetic object was recognized in the northeasternmost part of Slovakia within the area which is created by sediments of the Flysch belt. This is certain rarity because the Flysch sequence is practically without magnetic rocks. Due to this was obvious that anomaly is caused by an exotic rocks complex, intruded into Flysch sediments. The shape and the character of anomalous body indicated that source of anomaly is located in the shallow depth under surface relatively. The anomaly has been modelled in the 2D. Source of magnetic anomaly was interpreted as the product of Neogene volcanism – neck of intermediate rocks. Besides of this there were found out other minor anomalies within this area which might be caused also by smaller subvolcanic bodies. The Carpathian Conductivity Anomaly is located in the proximity of new observed magnetic anomalies. Due to this fact it is possible to open new view on the importance of this zone. In the case of justification of such interpretation the area might be interesting for its potential prognosis of hydrocarbons occurrence, metallogenetic prominence, as well as possibilities for underground storage of carbon dioxide.

Źródło:

Geological Quarterly; 2013, 57, 1; 123--134
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 44.

Tytuł:

Siliciclastic input into Upper Cenomanian synorogenic sediments of the High-Tatric Unit, Central Western Carpathians (Tatra Mountains); petrography, geochemistry and provenance

Autorzy:

Wolska, A.
Bąk, K.
Bąk, M.

Powiązania:

https://bibliotekanauki.pl/articles/2060546.pdf

Data publikacji:

2016

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

petrography
geochemistry
Upper Cenomanian
Zabijak Formation
High-Tatric Unit
Central Western Carpathians

Opis:

The Upper Cenomanian mixed siliciclastic-carbonate succession of the High-Tatric Unit was deposited during the initial stage of basinal closing of the Tatric area, part of the Zliechov (Križna) Basin (Inner Carpathian domain). As a result of tectonic activity taking place at the northern Veporic margin, pulses of siliciclastic input interrupted marine carbonate sedimentation. The siliciclastic material, part of the Zabijak Formation, has been studied along two sections (Pisana Gully and Zdziarski Gully) in the Western Tatra Mountains. Microfacies, petrographic and geochemical analyses reveal a variability of siliciclastic material composed of various types of granitoids and medium- or high-grade metamorphic rocks, with schists and gneisses. Such interpretation is confirmed by the results of elemental chemical analyses, in which immobile trace elements, such as REE, Th, Cr, Co, Zr, and Y were used as indices for sediment provenance. The parent rocks sustained moderate to intense chemical weathering, documented by chemical weathering indices (CIA, PIA, CIW, R). The weathering occurred in a humid climate with relatively high precipitation that caused strong leaching of particles. Chemical indices related to sorting processes suggest that the recycling of the source material was a minor significance. The siliciclastic input displays a waning upward tendency in the sections, which can be associated with diminishing of the source area by gradual inland progradation of a carbonate platform, caused by a global sea level rise during the Late Cenomanian.

Źródło:

Geological Quarterly; 2016, 60, 4; 919--934
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 45.

Tytuł:

Cretaceous and Eocene tectono-thermal events determined in the Inner Western Carpathians orogenic front Infratatricum

Autorzy:

Putiš, Marián
Danišík, Martin
Siman, Pawol
Nemec, Ondrej
Tomek, Čestmír
Ružička, Peter

Powiązania:

https://bibliotekanauki.pl/articles/2058652.pdf

Data publikacji:

2019

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Inner Western Carpathians
Infratatricum
orogenic wedge
tectono-thermal events
zircon fission track

Opis:

This paper re-assesses the tectono-thermal evolution of the frontal Infratatricum part of the Inner Western Carpathians orogen based on new geological-petrological and zircon fission track (ZFT) data and published 40Ar-39Ar and K-Ar data. The study area is in the Považský Inovec Mts. in Western Slovakia, where the Infratatric Inovec Nappe comprises a micaschist-gneiss basement and Upper Carboniferous-Lower Cretaceous cover with the Jurassic-Lower Cretaceous Humienec Succession; this latter is reconstructed from olistoliths in the Horné Belice Succession Upper Cretaceous flysch. The Infratatric Inovec Nappe posterior part is thrust over its frontal Humienec tectonic Slice with infolded Upper Cretaceous sediments. This nappe exhibits very low-temperature tectono-thermal overprinting, and this is documented by electron probe microanalysis of metamorphic phases and P-T estimates. The late Early Cretaceous age of this D1 stage event at approximately 115-95 Ma is recorded by 114 ±2 and 106 ±4 Ma phengitic white mica 40Ar-39Ar ages from a Lower Cretaceous cherty slate, and by 101 ±3 Ma 40Ar-39Ar age and 102 ±4 Ma ZFT age from Permian meta-sandstone. The Inovec Nappe was thus derived from an Albian-Early Cenomanian accretionary wedge. The hemipelagic Upper Turonian to Lower Santonian red marls and upward syn-orogenic Upper Santonian to Maastrichtian flysch were deposited on the frontal attenuated part of the Inovec Nappe-type basement in the inferred Pieninic-Váhic (~South-Penninic) zone. This flysch contains olistolithic to clastogeneous metamorphosed material, including the Lower Cretaceous slates, supplied from the posterior part of the Inovec Nappe. The 40Ar-39Ar age of 86 ±2 Ma from this nappes' Permian meta-sandstone is consistent with D2 thrusting at approximately 95-85 Ma and Horné Belice foreland flysch basin supply in the D3 stage at ~85-65 Ma. The Inovec Nappe frontal Humienec tectonic Slice with infolded Upper Cretaceous sediments suggests formation of a Paleocene-Eocene accretionary wedge at approximately 65-40 Ma in the D4 stage. This event is constrained by 40Ar-39Ar age of 48 ±2 Ma from the Tatricum hanging wall blastomylonites and whole-rock K-Ar age of 46 ±3 Ma from a Permian basalt olistolith in the footwall Infratatricum Horné Belice flysch. The Infratatricum finally became part of an Eocene accretionary wedge north of the Hrádok-Zlatníky thrust-fault, and reheating and exhumation cooling is documented by 57-37 Ma ZFT ages. Although the Infratatricum exhibits Late Cretaceous and Eocene tectono-thermal imprints, it is a remnant of the Early Cretaceous structure at the Inner Western Carpathian front. This imposes the Infratatricum as a distal continental margin of the Penninicum.

Źródło:

Geological Quarterly; 2019, 63, 2; 248--274
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 46.

Tytuł:

Eustatic and tectonic control on late Eocene fan delta development (Orava Basin, Central Western Carpathians)

Autorzy:

Starek, D.
Sliva, L’.
Vojtko, R.

Powiązania:

https://bibliotekanauki.pl/articles/2058980.pdf

Data publikacji:

2012

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Paleogene
Orava
Western Carpathians
fan delta
mass flow deposits
coarse-grained delta

Opis:

The evolution of the Central Carpathian Paleogene Basin (CCPB) reflects an important role of relative sea level changes on a tectonically active basin margin. After the initial upper Lutetian/Bartonian transgression, the next regressive-transgressive cycle played a key role in a formation of the late Eocene fan delta facies associations in the southern Orava region of Northern Slovakia. Detailed sedimentary analysis allowed the separation of the following three facies associations which represent distinct depositional environments: alluvial fan (subaerial fan delta; Unit 1); subaqueous fan delta (Unit 2); and prodelta/slope and basin (Unit 3). The first stage of delta development is connected with eustatic sea level fall at the Bartonian/Priabonian boundary, accompanied by subaerial exposure, fluvial incision and deposition of alluvial fan sediments. Subaerial deposition was characterized by a variety of mass flow conglomerates with a red muddy matrix, interfingering with stream or sheetflood deposits. The next stage of the delta corresponds to high-amplitude transgression related to rapid tectonic subsidence along the CCPB margins during the Priabonian. The vertical arrangement of facies suggests retrograde delta development that shows rapid submergence of the subaerial parts and onlap of subaqueous mass flow conglomerates, often reworked by waves or wave-induced shallow-marine currents. Continuous deepening of the depositional environment during the late Priabonian/early Rupelian led to the relatively rapid superposition of prodelta/slope and basin facies associations by slowly accumulated hemipelagic deposis.

Źródło:

Geological Quarterly; 2012, 56, 1; 67-84
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 47.

Tytuł:

Evolution of Late Cretaceous-Palaeogene synorogenic basins in the Pieniny Klippen Belt and adjacent zones (Western Carpathians, Slovakia) : tectonic controls over a growing orogenic wedge

Autorzy:

Plašienka, D.
Soták, J.

Powiązania:

https://bibliotekanauki.pl/articles/191730.pdf

Data publikacji:

2015

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

Western Carpathians
Oravic units
Gosau Supergroup
synorogenic sediments
palaeotectonic interpretation
geodynamic evolution

Opis:

The Pieniny Klippen Belt and neighbouring zones of the Western Carpathians represent an ancient accretionary wedge that developed during the meso-Alpidic (Coniacian–Eocene) tectonic epoch. After an overview of the extensive literature data, the authors present an interpretation of the synorogenic sedimentary record of these zones as being related to various environments of the foreland basin system consisting of the trench-foredeep and wedge-top depositional areas. The peripheral trench-foredeep depozones migrated from the South Penninic-Vahic oceanic realm towards the Oravic continental fragment in an intra-Penninic position, where the synorogenic deposits were laid down with coarsening- and thickening-upward trends before being overthrust by the propagating orogenic wedge tip. The development of wedge-top, piggyback basins (Gosau Supergroup) was controlled by the dynamics of the underlying wedge, composed of frontal elements of the Fatric and Hronic cover nappe systems of the Central Western Carpathians (Austroalpine units). Several compressional and extensional events are documented in the complex sedimentary and structural rock records within the wedge and related basins. The successive transgressive-regressive depositional cycles and corresponding deformation stages are interpreted in terms of a dynamic accretionary wedge that maintained the critical taper only transiently. The supercritical taper states are reflected in regression, shallowing and erosion in the wedge-top area, while the trench was supplied with large amounts of clastics by various gravity-flow types. On the other hand, the collapse stages tending to subcritical wedge taper are indicated by widespread marine transgressions or ingressions in the wedge-top area and a general deepening of all basins to bathyal conditions. Accordingly, the evolution of the entire trench-foredeep and wedge-top basin systems was principally controlled by the complex interplay of the regional tectonic evolution of the Alpine-Carpathian orogenic system, local wedge dynamics and eustatic sea-level fluctuations.

Źródło:

Annales Societatis Geologorum Poloniae; 2015, 85, 1; 43-76
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 48.

Tytuł:

The identification of neotectonics based on changes of valley floor width

Autorzy:

Bil, M.

Powiązania:

https://bibliotekanauki.pl/articles/294316.pdf

Data publikacji:

2002

Wydawca:

Stowarzyszenie Geomorfologów Polskich

Tematy:

Outer Western Carpathians
flysch
neotectonics
morphometry
topographic maps analysis
valley floor width

Opis:

This paper concerns the identification of neotectonics structures on the basis of topographic maps analysis. The investigation parameter is valley floor width (VFW), this being applied to the drainage basin of the BeCva river, Czech Republic. It is firstly necessary to determine the theoretic profile of the VFW downstream increment. For its construction the magnitudo was used (Shreve, 1966). Then, the differences between the real VFW and the theoretical VFW were calculated. The differences were classified according to the associated bedrock lithology. The sections where differences were widely divergent from the average are assumed to be have been affected by neotectonics.

Źródło:

Landform Analysis; 2002, 3; 77-85
1429-799X

Pojawia się w:

Landform Analysis

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 49.

Tytuł:

Wybrane problemy regionalizacji fizycznogeograficznej Centralnych Karpat Zachodnich

Autorzy:

Balon, Jarosław

Powiązania:

https://bibliotekanauki.pl/articles/634083.pdf

Data publikacji:

2012

Wydawca:

Uniwersytet Jagielloński. Wydawnictwo Uniwersytetu Jagiellońskiego

Tematy:

physicogeographical regionalization
Western Carpathians
physicogeographical border
regionalizacja fizycznogeograficzna
Karpaty Zachodnie
granica fizycznogeograficzna

Opis:

W artykule autor ukazuje cztery problemy regionalizacji fizycznogeograficznej w słowackiej części Karpat. Należą do nich: granica pomiędzy Małą Fatrą a Magurą Orawską, przynależność fizycznogeograficzna Szypskiej Fatry, przynależność fizycznogeograficzna Szczyrbskiego Działu oraz ranga taksonomiczna Gór Lewockich. Omówiono dotychczasowe rozwiązania tych problemów przez autorów polskich i słowackich, dokonano krytycznej ich oceny i zaproponowano nowe rozwiązania.
The author presents an attempt to solve several problems of physicogeographical divisions in the Slovak part of the Carpathians. Different regionalizations (Hromadka 1956, Kondracki 1978, Mazur, Lukniś 1978, 1982, Czeppe, German 1979, Balon et al. 1995, Balon, Jodłowski 2005) are discussed and then critically evaluated. New solutions proposed are based on the analysis of selected features of natural environment and guided by the principles described in the author’s other paper (Balon 2000). The new course of the border between the Mala Fatra and the Oravska Magura should be delineated along the line: Istebné – Istebnianka stream valley – the pass (865 m a.s.l.) between Mračkovo and Opálené – Plešivský stream valley. The physicogeographical status of the Šipska Fatra massif and the Chočské Vrchy was also the subject of the study. As a result of the analysis of the border between two basins, the Liptovska Kotlina and Spišska Kotlina, a separate physicogeographical region Štrbský Divide was distinguished. The physicogeographical status of the Levočske Vrchy was also taken into consideration. In the author’s opinion those mountains form a macroregion together with the Bachureň Mts. and parts of the Medzihorie Spišsko-Šarišské. Selected issues presented in the paper indicate a need for a more detailed (to the level of microregion) physicogeographical regionalization of the Central Western Carpathians.

Źródło:

Prace Geograficzne; 2012, 128; 29-43
1644-3586

Pojawia się w:

Prace Geograficzne

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 50.

Tytuł:

Morphotype variation of orthophragminids as a palaeoecological indicator: A case study of Bartonian limestones, Pod Capkami Quarry, Tatra Mts, Poland

Autorzy:

Machaniec, E.
Jach, R.
Gradziński, M.

Powiązania:

https://bibliotekanauki.pl/articles/191441.pdf

Data publikacji:

2011

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

Larger benthic foraminifera
orthophragminids
morphotype
transgression
palaeoenvironment
Eocene
Tatra Mts.
Western Carpathians

Opis:

Nummulites-Discocyclina bioclastic packstone and Discocyclina rudstone occur in the transgressive sequence of the Middle–Upper Eocene deposits in the Tatra Mts. The succession of the studied facies is a direct response to a rapid environmental change, related to progressive deepening. Facies transition from Nummulites- Discocyclina bioclastic packstone of proximal mid-ramp to Discocylina rudstone of distal mid- and outer-ramp is an exemplary record of a deposition during deepening conditions. Increasing of diversity of the genus Discocyclina, decreasing of diversity of other foraminifera up the section and vertical variation of orthophragminid mor- photypes from the ovate- through saddle- to the disc-shaped tests are related to deepening and shadowing of the depositional environment.

Źródło:

Annales Societatis Geologorum Poloniae; 2011, 81, No 2; 199-205
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 51.

Tytuł:

Facies and sedimentary environment of the carbonate-dominated Carpathian Keuper from the Tatricum domain: results from the Dolina Smytnia valley (Tatra Mts, Southern Poland)

Autorzy:

Jaglarz, P.

Powiązania:

https://bibliotekanauki.pl/articles/191920.pdf

Data publikacji:

2010

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

tectonics
climate
dolostones
palaeosols
uppermost Ladinian-Norian
High-Tatric Unit
Western Carpathians

Opis:

The paper focuses on an interpretation of sedimentary and early diagenetic environment in the carbonate-dominated uppermost Ladinian-Norian succession from the Tatricum domain of the Tatra Mountains as well as its controlling factors. Limestones with cherts are the product of pedogenic processes, formed during long-term exposures of carbonate substrate. Chalcedony cherts were formed during relatively early diagenesis of pedogenic limestones. Dolostones and dolomitic mudstones were deposited in a kind of salt marshes. Pseudomorphs after sulfates and absence of benthic fauna indicate increased salinity and intensive evaporation. Additionally, low TOC concentration suggests a low productivity in the basin. On the contrary, stable isotope signals indicate that the sedimentary environment was strongly affected by meteoric water. Moreover, 18O and concentration of Sr suggest that dolostones were formed under the influence of both marine and meteoric waters. Dolomitic mudstones could be deposited in a salt-marsh environment fed by distal sheet floods. Components of palynological material and organic compounds in black dolomitic mudstones indicate the terrestrial origin of organic matter. Dolomitic regoliths were formed as the result of subaerial exposure and karstification of dolostones. Coarse-grained siliciclastics and variegated mudstone are interpreted, respectively, as a fluvial channel and flood plain facies of ephemeric fluvial environment. Sedimentary environment of the Keuper sediments was controlled by two main factors: synsedimentary tectonic movements and climate changes. In the latest Ladinian, the Middle Triassic carbonate platform was emerged, what resulted in the development of palaeosols. Block tectonic movements affected the Tatricum Basin in Keuper time. Horsts were emerged, whereas troughs were filled with fluvial or salt marsh sediments. Intensive tectonic movements are suggested by seismic-generated slumps and abrupt facies changes. More intensive chemical weathering and intensive contribution of pure siliciclastics suggest climate pluvialization in late Ladinian-early Carnian time. On the contrary, domination of physical weathering indicates the aridization of climate in late Carnian?-Norian time. The upper Carnian?-Norian succession was formed in hot and semi-arid climate conditions. Long-term climate changes was masked by short-term climate fluctuations. Geochemical indicators suggest that dolostones represent more humid periods, whereas dolomitic mudstones relatively dry periods.

Źródło:

Annales Societatis Geologorum Poloniae; 2010, 80, No 2; 147-161
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 52.

Tytuł:

Walory szaty roślinnej otoczenia źródeł w Ustroniu i jej znaczenie dla ekoturystyki
Natural values of the vegetation of springs in Ustroń surroundings and its importance to ecotourism

Autorzy:

Wilczek, Z.
Zarzycki, W
Kulik, K.
Zimnol, J

Powiązania:

https://bibliotekanauki.pl/articles/949986.pdf

Data publikacji:

2014

Wydawca:

Polskie Towarzystwo Inżynierii Ekologicznej

Tematy:

uzdrowiska
źródła
ekoturystyka
bioklimat
Karpaty Zachodnie
spa
springs
ecotourism
bioclimate
Western Carpathians

Opis:

Ustroń jest miejscowością uzdrowiskową położoną na obszarze Karpat Zachodnich, w Polsce południowej, w przedziale wysokościowym 360–480 m n.p.m. Ze względu na bliskość Konurbacji Górnośląskiej (ok. 50 km) Ustroń jest masowo odwiedzany przez turystów. Obiektem badań było otoczenie trzech popularnych źródeł mineralnych: Źródła Karola, Źródła Żelazistego i Źródła na Równicy. Badania terenowe objęły analizę roślinności i spis flory w promieniu 100 metrów od każdego ze źródeł. Wyniki pokazują obecność 21 zbiorowisk roślinnych reprezentujących 8 klas roślinności oraz 167 gatunków roślin naczyniowych. Wiele z nich jest rzadkich i chronionych. Walory przyrodnicze obszaru badań mogą być wykorzystane do promocji ekoturystyki na obszarze Ustronia. Co więcej, każde zbiorowisko roślinne ma swój specyficzny wpływ na ludzkie zdrowie i lokalne warunki bioklimatyczne, więc analiza roślinności powinna być potraktowana jako niezbędna dla każdej miejscowości uzdrowiskowej.
Ustroń is a spa town in Southern Poland in area of the Western Carpathians (attitude range: 360–480 m a.s.l.). It is very popular with tourists due to its proximity to biggest urban area of Poland – Upper Silesian Metropolis (about 50 km). The objects of study were surroundings of 3 popular mineral springs in Ustroń: Karol Spring, Ferruginous Spring and Spring on Równica Hill. Field research concerned vegetation and flora within 100 m of each spring. Results show occurrence of 21 different vegetation types from 8 vegetation classes and 167 vascular species. Many of them are rare and legal protected. Natural values of study area could be use in promotion of ecotourism in Ustroń. What more, each plant community have specific influence to a human health and local bioclimatic properties, so it is necessary to recognize vegetation of spa towns.

Źródło:

Inżynieria Ekologiczna; 2014, 40; 173-182
2081-139X
2392-0629

Pojawia się w:

Inżynieria Ekologiczna

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 53.

Tytuł:

Late Jurassic-Miocene evolution of the Outer Carpathian fold-and-thrust belt and its foredeep basin (Western Carpathians, Poland)

Autorzy:

Oszczypko, N.

Powiązania:

https://bibliotekanauki.pl/articles/2058934.pdf

Data publikacji:

2006

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Outer Western Carpathians
rifting
inversion
subsidence
tectono-sedimentary evolution
peripheral foreland basin

Opis:

The Outer Carpathian Basin domain developed in its initial stage as a Jurassic-Early Cretaceous rifted passive margin that faced the eastern parts of the oceanic Alpine Tethys. Following closure of this oceanic basin during the Late Cretaceous and collision of the Inner Western Carpathian orogenic wedge with the Outer Carpathian passive margin at the Cretaceous-Paleocene transition, the Outer Carpathian Basin domain was transformed into a foreland basin that was progressively scooped out by nappes and thrust sheets. In the pre- and syn-orogenic evolution of the Outer Carpathian basins the following prominent periods can be distinguished: (1)Middle Jurassic- Early Cretaceous syn-rift opening of basins followed by Early Cretaceous post-rift thermal subsidence, (2) latest Cretaceous- Paleocene syn-collisional inversion, (3) Late Paleocene toMiddle Eocene flexural subsidence and (4) Late Eocene-EarlyMiocene synorogenic closure of the basins. In the Outer Carpathian domain driving forces of tectonic subsidence were syn-rift and thermal post-rift processes, as well as tectonic loads related to the emplacement of nappes and slab-pull. Similar to other orogenic belts, folding of the Outer Carpathians commenced in their internal parts and progressed in time towards the continental foreland. This process was initiated at the end of the Paleocene at the Pieniny Klippen Belt/Magura Basin boundary and was completed during early Burdigalian in the northern part of the Krosno Flysch Basin. During Early and Middle Miocene times the Polish Carpathian Foredeep developed as a peripheral foreland basin in front of the advancing Carpathian orogenic wedge. Subsidence of this basin was controlled both by tectonic and sedimentary loads. The Miocene convergence of the Carpathian wedge with the foreland resulted in outward migration of the foredeep depocenters and onlap of successively younger deposits onto the foreland.

Źródło:

Geological Quarterly; 2006, 50, 1; 169-194
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 54.

Tytuł:

A contribution to the snowbed liverwort flora of the Tatra Mountains (Western Carpathians, Poland and Slovakia)

Autorzy:

Gorski, P.

Powiązania:

https://bibliotekanauki.pl/articles/790517.pdf

Data publikacji:

2015

Wydawca:

Uniwersytet Przyrodniczy w Poznaniu

Tematy:

contribution
snow bed
liverwort
flora
Tatras Mountains
Western Carpathians Mountains
Polska
Slovakia

Opis:

The article is a first update of the list of liverwort localities published in A synopsis of liverworts occurring in the Tatra Mountains (Western Carpathians, Poland and Slovakia): checklist, distribution, and new data (Górsk i & Váňa 2014). It presents localities of 19 liverwort species collected during 2003–2014 in snowbeds in the entire area of the Tatra Mts. Moreover, for some species, localities from habitats other than snowbeds were given. Localities of the following liverworts are presented: Anthelia juratzkana, Cephalozia ambigua, C. bicuspidata, Diplophyllum taxifolium, Fuscocephaloziopsis albescens [= Pleurocladula albescens], Gymnocolea inflata, Gymnomitrion adustum [= Marsupella adusta], G. concinnatum, G. brevissimum [= Marsupella brevissima], Lophozia wenzelii, Marsupella boeckii, M. condensata, M. emarginata, M. sprucei, Moerckia blyttii, Nardia scalaris, Pseudolophozia sudetica [= Lophozia sudetica], Schistochilopsis opacifolia [= Lophozia incisa subsp. opacifolia] and Trilophozia quinquedentata [= Tritomaria quinquedentata].

Źródło:

Steciana; 2015, 19, 3
1689-653X

Pojawia się w:

Steciana

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 55.

Tytuł:

Loess-like silts in the Beskid Mały and Beskid Makowski Mountains, Western Outer Carpathians

Autorzy:

Grzybowski, K.

Powiązania:

https://bibliotekanauki.pl/articles/2059330.pdf

Data publikacji:

2001

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Western Outer Carpathians
Quaternary
loess-like silts
stratigraphy

Opis:

Among the Quaternary deposits of the Beskid Mały and Beskid Makowski Mts. in southern Poland, loess-like silts occurring in the Skawa River valley and the Paleczka River valley are distinguishable by their high loess index values as well as by the presence of amphibole grains and by notable amounts of biotite grains. These silts originated by aeolian sedimentation during the younger Pleniglacial of the Vistulian, corresponding to the Younger Upper Loess. The amphibole and most of the biotite was derived from deflation of a glaciofluvial cover in the Carpathian forelands and Fore-Carpathian basins. They indicate the importance of northern winds in the Plenivistulian atmospheric circulation.

Źródło:

Geological Quarterly; 2001, 45, 1; 67-74
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 56.

Tytuł:

Integrated stratigraphy of the Middle–Upper Jurassic of the Krížna Nappe, Tatra Mountains

Autorzy:

Jach, R.
Djerić, N.
Goričan, Š.
Řeháková, D.

Powiązania:

https://bibliotekanauki.pl/articles/191333.pdf

Data publikacji:

2014

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

carbon and oxygen isotopes
radiolarians
calcareous dinoflagellates
radiolarites
Krizna nappe
Western Carpathians
Tethys

Opis:

Middle-Upper Jurassic pelagic carbonates and radiolarites were studied in the Krížna Nappe of the Tatra Mountains (Central Western Carpathians, southern Poland and northern Slovakia). A carbon isotope stra- tigraphy of these deposits was combined with biostratigraphy, based on radiolarians, calcareous dinoflagellates and calpionellids. In the High Tatra and Belianske Tatra Mountains, the Bajocian and part of the Bathonian are represented by a thick succession of spotted limestones and grey nodular limestones, while in the Western Tatra Mountains by relatively thin Bositra-crinoidal limestones. These deposits are referable to a deeper basin and a pelagic carbonate platform, respectively. The various carbonate facies are followed by deep-water biosiliceous facies, namely radiolarites and radiolarian-bearing limestones of Late Bathonian-early Late Kimmeridgian age. These facies pass into Upper Kimmeridgian-Lower Tithonian pelagic carbonates with abundant Saccocoma sp. The bulk-carbonate isotope composition of the carbonate-siliceous deposits shows positive and negative S C excursions and shifts in the Early Bajocian, Late Bajocian, Early Bathonian, Late Bathonian, Late Callovian, Middle Oxfordian and Late Kimmeridgian. Additionally, the S13C curves studied show a pronounced increasing trend in the Callovian and a steadily decreasing trend in the Oxfordian-Early Tithonian. These correlate with the trends known from the Tethyan region. The onset of Late Bathonian radiolarite sedimenlalion is marked by a decreasing trend in S13C. Increased S13C values in the Late Callovian, Middle Oxfordian and Late Kimmeridgian (Moluccana Zone) correspond with enhanced radiolarian production. A significant increase in CaCO3 content is recorded just above the Late Callovian S13C excursion, which coincides with a transition from green to variegated radiolarites.

Źródło:

Annales Societatis Geologorum Poloniae; 2014, 84, 1; 1-33
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 57.

Tytuł:

Sedimentology of the Godula Formation in the Moravskoslezské Beskydy Mts. (Outer Western Carpathians, Czech Republic)

Autorzy:

Maceček, Lukáš

Powiązania:

https://bibliotekanauki.pl/articles/1835969.pdf

Data publikacji:

2021

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

facies analysis
turbidite systems
siliciclastic deposits
Outer Western Carpathians
Moravskoslezské Beskydy Mts.
Cretaceous

Opis:

The present account summarizes the results of lithological and facies analysis of representative sections of the Godula Formation, in order to contribute to the understanding of the lithofacies structure of this formation, the processes involved in its development and the character of the depositional environment. The sedimentology of different parts of the Godula Formation was investigated in six representative sections in the western and central parts of the Moravskoslezské Beskydy Mts. The Godula Formation is made up mainly of Upper Cretaceous siliciclastic turbidites and was formed during the most significant depositional phase of the filling of the deep-sea Silesian Basin. On the basis of sedimentological research, five facies classes (including four subclasses) were defined: 1) conglomeratic sandstones, 2) sandstones, 3) sandstones with mudstones, 4) mudstones with sandstones and siltstones, and 5) mudstones with siltstones. The methodology of facies analysis allowed the identification of several facies association, corresponding to the medial and distal parts of a turbidite fan and associated siliciclastic apron. The facies of depositional lobes, lobe transitions and the apron are described. The sandstone and mudstone facies (F3) occurs mostly in the depositional lobes. The sandstone facies (F2) and mudstone with sandstone and siltstone facies (F4) are present only to a lesser degree. The facies of the lobe transitions include lithologic associations of the lobe fringe and channel levee environments. They comprise mainly the mudstones with sandstones and siltstones (F4) and the mudstone with siltstone facies (F5). In the apron deposits, the sandstone facies (F2) and the conglomeratic sandstone facies (F1) predominate. Palaeocurrent analysis from measurements made in selected profiles showed that in the Moravskoslezské Beskydy Mts., the dominant direction of sediment transport was from SW to NE. After applying correction of the known counterclockwise rotation of the nappes of the Outer Carpathians, this corresponds to a longitudinal direction along the original axis of the basin.

Źródło:

Annales Societatis Geologorum Poloniae; 2021, 91, 3; 309-325
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 58.

Tytuł:

Stratigraphic position of alkaline volcanic rocks in the autochthonous cover of the High-Tatric Unit (Western Tatra Mts., Central Western Carpathians, Slovakia)

Autorzy:

Madzin, J.
Sýkora, M.
Soták, J.

Powiązania:

https://bibliotekanauki.pl/articles/2059966.pdf

Data publikacji:

2014

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Central Western Carpathians
Western Tatra Mountains
autochthonous cover of the High-Tatric Unit
alkaline volcanism
biostratigraphy

Opis:

Biostratigraphic investigations of carbonate strata that sandwich volcanic rocks and studies of the volcanic rocks were made along five composite lithological sections across the Upper Jurassic-Lower Cretaceous carbonate rocks of autochthonous cover of the High-Tatric Unit in the Osobitá peak area of the Western Tatra Mts. A carbonate microbreccia that consists almost exclusively of limestone clasts containing calpionellids occurs immediately below the volcanics. The youngest identified microfossil Calpionella elliptica Cadisch in the individual limestone clasts showed the age of breccia formation to be younger than late Early-early Middle Berriasian. The volcanic rocks are overlain by the Osobitá Limestone Formation, which in the lowermost horizons consists of a few metres thick crinoidal limestone containing the foraminifers Meandrospira favrei (Charollais, Brönnimann & Zaninetti), Sabaudia minuta Hofker and Montsalevia salevensis (Charollais, Brönnimann & Zaninetti) indicating a Late Valanginian-Early Hauterivian age. The biostratigraphical and sedimentological data obtained show that volcanism took place in several phases. Less intense phases of volcanism are recorded as thin tuffitic laminae within the upper parts of the Tithonian-early Mid Berriasian Sobótka Limestone Member and as fragments of volcanic rock in the carbonate breccia. The main phase(s) of volcanism took place during the Late Berriasian-?Early Valanginian.

Źródło:

Geological Quarterly; 2014, 58, 1; 163--180
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 59.

Tytuł:

Modelowania sejsmiczne - narzędzie wspomagające strukturalną interpretację danych sejsmicznych z rejonu Karpat zewnętrznych pomiędzy Babią Górą a Wadowicami
Seismic modelling - a support tool for structural interpretation of seismic data from the area of the Outer Carpathians between Babia Góra and Wadowice

Autorzy:

Pietsch, K.
Kobylarski, M.
Urban, A.

Powiązania:

https://bibliotekanauki.pl/articles/183875.pdf

Data publikacji:

2007

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

Karpaty Zachodnie
sejsmiczna interpretacja strukturalna
modelowanie sejsmiczne
Western Carpathians
seismic structural interpretation
seismic modelling

Opis:

Złożona budowa Karpat powoduje, że sejsmiczny obraz jest bardzo trudny do interpretacji. Wiarygodne odtworzenie układu strukturalnego utworów platformowego podłoża wymaga zastosowania dwuwymiarowych modelowań sejsmicznych. Przedstawiono wykorzystanie modelowań sejsmicznych do interpretacji profilu 56-1-89K, zarejestrowanego w obszarze struktury Stryszawa, w zachodniej części Karpat zewnętrznych. Modele sejsmogeologiczne opracowano z wykorzystaniem danych otworowych (Lachowice 7 i Ślemień 1) oraz wstępnie zinterpretowanego profilu 56-1-89K. Teoretyczne przekroje czasowe obliczono z wykorzystaniem programu Outrider oraz systemu Omega. Geologiczna interpretacja, wykonana z wykorzystaniem wyników modelowań sejsmicznych, umożliwiła odtworzenie horyzontów JSsp, Flsp, PALstr=Msp, Cm+D1str i Pr oraz wiarygodną identyfikację uskoków ograniczających strukturę Stryszawy.
The complex structure of the Carpathians, causes that seismic pattern is very difficult. The reliable reconstruction of the structural system of the platform basement formations require application of 2D seismic modelling. The paper presents the application of seismic modelling for interpretation of the 56-1-89K profile, recorded in the Stryszawa structure area, in the western part of the Outer Carpathians. Seismogeological models were developed using borehole data (Lachowice 7 and Ślemień 1) and the preliminary interpreted 56-1-89K profile. Theoretical time sections were computed with the softwares: Outrider and Omega. Geological interpretation performed using results of seismic modeling enabled the reconstruction of JSsp, Flsp, PALstr=Msp, Cm+D1str and Pr horizons and reliable identification of faults limiting the Stryszawa structure.

Źródło:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2007, 33, 4/1; 183-196
0138-0974

Pojawia się w:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 60.

Tytuł:

Results of archaeological rescue excavations at Mucharz (Beskidy Mts.)

Autorzy:

Valde-Nowak, Paweł
Tarasiński, Arkadiusz

Powiązania:

https://bibliotekanauki.pl/articles/442466.pdf

Data publikacji:

2010

Wydawca:

Uniwersytet Jagielloński. Instytut Archeologii

Tematy:

Western Carpathians
Mucharz site
rescue excavations
Świdry culture
Mesolithic
Neolithic
Mierzanowice culture
Medieval Period

Opis:

During rescue excavations at the site Mucharz 12 carried out due to building of the water reservoir at Świnna Poręba on the border of the Middle and Small Beskidy Mts. unexpectedly traces of the Late Paleolithic settlement of Świdry culture were discovered, among them remains of two dwelling features. Besides them the site provided numerous Mesolithic artifacts, traces of Neolithic settlement, assemblages representing two different variants of Bronze Age Mierzanowice culture and finally remains connected with medieval occupation. Studies on stone artifacts demonstrated that mainly during the Mesolithic period local deposits of Mikuszowice hornstone were exploited. Presence of the artifacts made of raw materials coming from some distance sources (e.g. Jurassic flint) was confirmed as well. Presented results put new light on the problem of detectability of archaeological sites within mountain zones of southern Poland, as well as on the character of prehistorical settlement traces on the territory.

Źródło:

Recherches Archéologiques Nouvelle Serie; 2010, 2; 185-201
0137-3285

Pojawia się w:

Recherches Archéologiques Nouvelle Serie

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 61.

Tytuł:

Macroconch ammonites from the Štramberk Limestone deposited in the collections of the Czech Geological Survey (Tithonian, Outer Western Carpathians, Czech Republic)

Autorzy:

Vašíček, Zdeněk
Malek, Ondřej

Powiązania:

https://bibliotekanauki.pl/articles/2060948.pdf

Data publikacji:

2019

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

megaammonites
Tithonian
Silesian Unit
Outer Western Carpathians
megaaminity
tytanian
jednostka śląska
Zewnętrzne Karpaty Zachodnie

Opis:

11 specimens of large sized ammonites from the Štramberk Limestone deposited in the collections in Prague represent 6species. Two species belong to the superfamily Lytoceratoidea, the remaining ones to the superfamily Perisphinctoidea. The perisphinctid specimens belong to the Lower and the Upper Tithonian, and the lytoceratids probably correspond to the same stratigraphic level. Two species, namely Ernstbrunnia blaschkei and Djurjuriceras mediterraneum were not known from the Štramberk Limestone earlier.

Źródło:

Volumina Jurassica; 2019, 17, 1; 81--94
1896-7876
1731-3708

Pojawia się w:

Volumina Jurassica

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 62.

Tytuł:

Pierwsze stanowisko holoceńskich uskoków w polskich Karpatach zewnętrznych
First site of Holocene faults in the Polish Outer Carpathians

Autorzy:

Zuchiewicz, W.
Tokarski, A. K.
Świerczewska, A.
Zasadni, J.
Siemińska, A.

Powiązania:

https://bibliotekanauki.pl/articles/2074880.pdf

Data publikacji:

2011

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

holoceńskie zaburzenie uskokowe
neotektonika
Zewnętrzne Karpaty Zachodnie
Polska
Holocene faulting
neotectonics
Outer Western Carpathians
Polska

Opis:

The paper presents the first example of Holocene faults in the OuterWestern Carpathians in Poland. Small-scale normal faults at Koninki, Gorce Mts., cut both Palaeocene strata of the Ropianka Formation of the Magura Nappe and overlying coarse-clastic bedload facies of Holocene alluvium that builds a 5-5.5-high terrace step of a small valley. These NE-trending faults are accompanied by reorientation of clast a-b planes subparallel to fault planes and by clast fracturing. Such deformations must have been induced by relatively strong earthquakes, unknown from historical record of the Outer Carpathian seismicity. Fault attitude points to NW-oriented axis of the minimum principal stress, which is compatible with parameters of the present-day stress field in the Outer Western Carpathians of Poland.

Źródło:

Przegląd Geologiczny; 2011, 59, 8; 566-575
0033-2151

Pojawia się w:

Przegląd Geologiczny

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 63.

Tytuł:

Late Albian calcareous dinocysts and calcitarchs record linked to environmental changes during the final phase of OAE 1d – a case study from the Tatra Mountains, Central Western Carpathians

Autorzy:

Ciurej, A.
Bąk, K.
Bąk, M.

Powiązania:

https://bibliotekanauki.pl/articles/2060589.pdf

Data publikacji:

2017

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

calcareous dinocysts
palaeoecology
upper Albian
Oceanic Anoxic Event 1d
Tatra Mts.
Central Western Carpathians

Opis:

Calcareous dinocysts and calcitarchs have been investigated for the first time within the Upper Albian limestone and marl succession of the Zabijak Formation from the High-Tatric Unit in the Tatra Mountains (Central Western Carpathians), related to the Oceanic Anoxic Event 1d (OAE 1d). Four groups of morphotaxa of calcareous dinocysts have been distinguished. They totally dominate the assemblages, and belong to the pithonellids. They are represented by Pithonella sphaerica (Kaufmann in Heer) and P. ovalis (Kaufmann in Heer), which dominate, as well as P. trejoi Bonet and P. lamellata Keupp in Keupp and Kienel, which are less abundant. Two other morphotaxa, Colomisphaera gigantea (Borza) and Cadosina oraviensis Borza, occur sporadically in the assemblages. Both forms represent the calcitarch group, which assembled calcispheres of unknown taxonomic affinity. The calcareous dinocyst and calcitarch diversity is low to moderate, compared to the general species richness known from Late Albian assemblages in other Western Tethyan sections. This is interpreted as a result of nutrient input fluctuations due to changes in the circulation pattern of surface and intermediate waters. The changes in the P. sphaerica/P. ovalis ratio along the Upper Albian section are here correlated with short-term (third-order) sea level fluctuations including transgressive and regressive events and a highstand. Pelletization processes might have influenced cyst abundance on the sea floor, especially during periods with oligotrophic surface waters.

Źródło:

Geological Quarterly; 2017, 61, 4; 887--895
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 64.

Tytuł:

Tectonics of the Beskid Wyspowy Mountains (Outer Carpathians, Poland)

Autorzy:

Konon, A.

Powiązania:

https://bibliotekanauki.pl/articles/2059276.pdf

Data publikacji:

2001

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Western Outer Carpathians
Magura Nappe
brachysynclines
mesostructures
block rotation
paleostresses

Opis:

The structure of the Magura Nappe, within the zone of maximal bending of the Western Outer Carpathians, is described; investigations were concentrated mainly in the Beskid Wyspowy Subunit. A zone, bounded to the north and south by duplexes, comprises large characteristic synclines (Snieznica, Lubogoszcz, Szczebel, Klimas, Lopien, Cwilin, Lubon Wielki). These appear on maps as isolated "island mountains", in the Beskid Wyspowy Subunit. These synclines contrast strongly with the belt-like distribution of regional folds to the west and east of the area. The synclinal massifs developed gradually. Fold belts several hundred metres long developed in the first phase of overthrusting of the Magura Nappe, with horizontal N-S compression dominant. Thrusts separating the individual subunits developed when the face of the overthrusting Magura Nappe stopped and the stress continued to push its southern parts forwards. The next phase, with continuing horizontal N-S stress included the development of strike-slip faults and the bending of the Carpathian Arc, resulting in extension of this part of the orogen. The syncline zone within the Beskid Wyspowy Subunit underwent disintegration and particular blocks became independent. Rotation of blocks with individual synclines took place along fault zones. In the part of the Polish Outer Carpathians investigated this stage is also characterised by a change of compression from N-S to NNE-SSW. Due to the uplift of this part of the Carpathians, strike-slip faults changed into dip-slip faults in the terminal part of this phase. reconstruction.

Źródło:

Geological Quarterly; 2001, 45, 2; 179-204
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 65.

Tytuł:

Slope instability hazard evaluation and landslide sites monitoring in the western Flysch Carpathians (Czech Republic)

Autorzy:

Baroň, I.
Krejčí, O.

Powiązania:

https://bibliotekanauki.pl/articles/1182919.pdf

Data publikacji:

2005

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

osuwiska
geozagrożenia
ocena zagrożeń
litologia
geomorfologia
Karpaty Zachodnie
landslides
geohazards
risk evaluation
lithology
geomorphology
Western Carpathians

Opis:

W lipcu 1997 roku obfite deszcze spowodowały ruchy zboczowe, zwłaszcza utworów fliszowych, w północno-wschodnich Czechach. Kompleksy mezozoiczne i trzeciorzędowe Zachodnich Karpat fliszowych charakteryzują się wysoczyznami i rzeźbą górską, głównie o charakterze erozyjnym i strukturalno-denudacyjnym. Obecnie jest realizowany projekt badawczy, podsumowujący dotychczasowe obserwacje, mający na celu ocenę wpływu morfologii i mechanizmów uruchamiających zjawiska osuwiskowe na obszarach modelowych. Każde lokalne osuwisko, poza oddziaływaniami przyrodniczymi, było także poddane działalności ludzkiej. Do badań wykorzystano kartografię geomorfologiczną, wiercenia rdzeniowe oraz badania geofizyczne. Wiek osuwisk określono na podstawie datowania metodą 14C oraz badaniami palinologicznymi, paleomagnetycznymi i archeologicznymi. W wyniku przeprowadzonych badań ustalono geometrię, mechanizmy oraz możliwy rozwój różnego typu osunięć zboczy. Rejestrację osuwisk prowadzono elektronicznie, duże tereny osuwiskowe dokładnie badano, a wyniki tych badań nanoszono na mapy w skali 1:10 000. Obszary te zostały sklasyfikowane w zależności od stopnia zagrożenia oraz intensywności występowania osuwisk. Mapy prezentujące warunki stabilności terenu stanowią podstawę do tworzenia map zagrożeń osuwiskami. Ocena stabilności terenu, morfologii, warunków geologicznych i hydrogeologicznych pozwala na wyznaczanie quasi-jednorodnych stref o określonym stopniu zagrożenia osuwiskami. Mapy takie wykorzystują władze administracyjne przy tworzeniu planów regionalnych i miejskich.

Źródło:

Polish Geological Institute Special Papers; 2005, 20; 9--13
1507-9791

Pojawia się w:

Polish Geological Institute Special Papers

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 66.

Tytuł:

Struktura nasunięcia karpackiego i jego podłoża w polskich Karpatach Zachodnich w świetle reinterpretacji wybranych regionalnych profili magnetotellurycznych
The structure of the Carpathian overthrust and its basement in the Polish Western Carpathians in the light of reinterpretation of selected regional magnetotelluric profiles

Autorzy:

Stefaniuk, M.
Klityński, W.
Jarzyna, J.
Golonka, J.

Powiązania:

https://bibliotekanauki.pl/articles/183829.pdf

Data publikacji:

2007

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

Karpaty Zachodnie
badania regionalne
sondowania magnetotelluryczne
podłoże
tektonika
Western Carpathians
regional survey
magnetotelluric sounding
basement
tectonics

Opis:

Przedmiotem artykułu są wyniki reinterpretacji trzech regionalnych profili magnetotellurycznych zlokalizowanych w polskich Karpatach Zachodnich. Badania magnetotelluryczne w tym obszarze wykonało Przedsiębiorstwo Badań Geofizycznych w Warszawie w latach 1997-2002, Prace reinterpretacyjne poprzedzone zostały przez analizę danych pomiarowych i ich reprocessing dla wybranych sondowań. W reinterpretacji wykorzystano głównie automatyczną inwersję 2D oraz inwersję 1D przy użyciu algorytmów Occama i LSQ. Dwuwymiarowe przekroje oporności opracowane na podstawie wyników automatycznej inwersji 2D oraz interpretacji 1D wykorzystano do konstrukcji modeli geoelektryczno-geologicznych. W interpretacji geologicznej wykorzystano także informacje geologiczne i wiertnicze oraz dane sejsmiki refleksyjnej.
The subject of the paper includes results of reinterpretation of three regional magnetotelluric profiles located in the western part of the Polish Carpathians. Magnetotelluric survey in the area was made by the Geophysical Exploration Company, Warsaw, in the years 1997-2002. Reinterpretation works were proceeded by analysis of measurement data and reprocessing for some soundings. Automatic 2D inversion and 1D inversion with the use of Occam and LSQ algorithms were employed in reinterpretation process. 2D resistivity sections obtained based on results of automatic 2D and 1D data interpretation were used to construct geoelectric and geologic models. Geological and borehole data, and reflection seismic data were also applied in geological interpretation.

Źródło:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2007, 33, 4/1; 143-166
0138-0974

Pojawia się w:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 67.

Tytuł:

Floristic diversity of the „Laki w Komborni” Natura 2000 site PLH180042 (Western Carpathians)

Autorzy:

Ziaja, M.
Wojcik, T.

Powiązania:

https://bibliotekanauki.pl/articles/790635.pdf

Data publikacji:

2017

Wydawca:

Uniwersytet Przyrodniczy w Poznaniu

Tematy:

floristic diversity
Laki w Komborni area
Western Carpathians Mountains
Natura 2000 area
meadow
vascular plant
Polska

Opis:

The vascular flora in the “Łąki w Komborni” Natura 2000 site comprises 219 species representing 44 families and 147 genera. Species from the families Asteraceae, Poaceae, Lamiaceae, Fabaceae, Rosaceae, Polygonaceae, Cyperaceae, Apiaceae, and Ranunculaceae were found to dominate. A geographical and historical analysis of species confirmed the clear dominance of apophytes (84%) over anthropophytes (16%) as well as perennials (69%) over short-lived (23%) species. The biological spectrum was dominated by hemicryptophytes (54%) and therophytes (19%), compared with other life forms. In terms of synecology, the flora was mainly represented by species from the classes Molinio-Arrhenatheretea, Stellarietea mediae, Artemisietea vulgaris and Phragmitetea. The “Łąki w Komborni” site is a habitat for 82 (37%) medicinal species and 155 (70%) forage species for bees. Noteworthy is the occurrence of protected species, e.g. Gladiolus imbricatus, Trollius europaeus, Centhaurium erythraea, Dactylorhiza majalis, Platanthera bifolia and Primula elatior.

Źródło:

Steciana; 2017, 21, 2
1689-653X

Pojawia się w:

Steciana

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 68.

Tytuł:

Analiza gęstości i porowatości z badań laboratoryjnych oraz wyników pomiarów otworowych i obliczeń w programie Estymacja w wybranych otworach w Karpatach Zachodnich
Analysis of density and porosity measurements on cores and results of density log and Estymacja calculations in the selected wells in the West Carpathians

Autorzy:

Jarzyna, J.

Powiązania:

https://bibliotekanauki.pl/articles/183848.pdf

Data publikacji:

2007

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

gęstość
porowatość
badania laboratoryjne
profilowania geofizyki otworowej
Karpaty Zachodnie
density
porosity
laboratory tests
well logs
Western Carpathians

Opis:

Wykonano analizę zmian gęstości i porowatości w wybranych otworach Karpat Zachodnich. Wykorzystano wyniki badań laboratoryjnych z bazy PITAKA Polskiego Górnictwa Naftowego i Gazownictwa S.A. oraz otworowe profilowania gęstościowe i wyniki obliczenia gęstości programem Estymacja, a także dane dotyczące kilkudziesięciu próbek poddanych badaniom porozymetrycznym. Zaobserwowano zgodność wyników pochodzących z różnych źródeł. Zestawienie danych dotyczących rożnych formacji litostratygraficznych w grupach otworów z tego samego rejonu pozwoliło na wzajemne uzupełnienie informacji. Charakterystyka gęstościowa formacji litostratygraficznych została wykorzystana do modelowania grawimetrycznego. Porowatość i gęstość zostały włączone do utworzenia zgeneralizowanych modeli własności fizycznych wybranych formacji litostratygraficznych w Karpatach Zachodnich.
The analysis of density and porosity changes was made for selected wells from the Western Carpathians. Laboratory data from the PITAKA database of the Polish Oil and Gas Company together with density logs and density values obtained from the Estymacja calculation as well as data for a few dozen samples from mercury porosimetry measurements were used. The agreement of results from different sources was observed. Data for different lithostratigraphic formations were set together for groups of wells from the same region. This enabled information to be mutually supplemented. Density characteristics of lithostratigraphic formations was used for gravity modeling. Porosity and density were employed to create generalized models of physical properties of selected lithostratigraphic formations form the Western Carpathians.

Źródło:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2007, 33, 4/1; 39-58
0138-0974

Pojawia się w:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 69.

Tytuł:

The Jurassic–Cretaceous transition in the High-Tatric succession (Giewont Unit, Western Tatra Mts, Poland): integrated stratigraphy and microfacies

Autorzy:

Lodowski, Damian Gerard
Pszczółkowski, Andrzej
Wilamowski, Andrzej
Grabowski, Jacek

Powiązania:

https://bibliotekanauki.pl/articles/2023960.pdf

Data publikacji:

2021

Wydawca:

Polska Akademia Nauk. Czytelnia Czasopism PAN

Tematy:

microfossils
rock magnetism
carbon isotopes
Western Carpathians
Tatra Mountains
mikroskamieniałości
skała magnetyczna
izotopy węgla
Karpaty Zachodnie
Tatry

Opis:

Herein are presented the results of detailed bio - (calcareous dinocysts, calpionellids, foraminifers, saccocomids) and chemostratigraphic (δ13C) studies combined with high-resolution microfacies, rock magnetic and gamma-ray spectrometry (GRS) investigations performed on the upper Kimmeridgian-upper Valanginian carbonates of the Giewont succession (Tatricum, Giewont and Mały Giewont sections, Western Tatra Mountains, Poland). The interval studied covers the contact between the Raptawicka Turnia Limestone (RTL) Fm. and the Wysoka Turnia Limestone (WTL) Fm. Their sedimentary sequence is composed of micrites, pseudonodular limestones, cyanoid packstones, lithoclastic packstone and encrinites. A precise correlation with the previously published Mały Giewont section is ensured by biostratigraphy, rock magnetic and GRS logs. The methodology adopted has enabled the recognition of two stratigraphic discontinuities, approximated here as corresponding to the latest Tithonian-early (late?) Berriasian and the early Valanginian. The hiatuses are evidenced by biostratigraphic data and the microfacies succession as well as by perturbations in isotopic compositions and rock magnetic logs; they are thought to result from a conjunction of tectonic activity and eustatic changes. A modified lithostratigraphic scheme for the Giewont and the Osobita High-Tatric successions is proposed. The top of the RTL Fm. falls in the upper Tithonian, where cyanoid packstones disappear. At the base of the WTL Fm. a new Giewont Member is defined as consisting of a basal lithoclastic packstone and following encrinites.

Źródło:

Acta Geologica Polonica; 2022, 72, 1; 107--135
0001-5709

Pojawia się w:

Acta Geologica Polonica

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 70.

Tytuł:

Corals from the Stramberk Limestone (Silesian Unit, Outer Western Carpathians, Czech Republic

Autorzy:

Eliasova, H.

Powiązania:

https://bibliotekanauki.pl/articles/184029.pdf

Data publikacji:

2008

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

koralowce
Karpaty Zachodnie
Karpaty zewnętrzne
corals
Outer Western Carpathians
Stramberk Limestone
Scleractinian corals
Late Tithonian/Early Berriasian

Opis:

The submitted contribution informs about the present-day situation of the coral fauna occurring in the Stramberk Limestone at the Kotouc Quarry near Stramberk. 120 determined species belong to 50 genera that pertain to 7 suborders of order Scleractinia

Źródło:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2008, 34, 3/1; 151-160
0138-0974

Pojawia się w:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 71.

Tytuł:

Monitoring geodynamic processes using geodetic and gravimetric methods: an example from the Western Carpathians (South Poland)
Monitoring procesów geodynamicznych z wykorzystaniem metod geodezyjnych i grawimetrycznych: przykład z Karpat Zachodnich (Polska południowa)

Autorzy:

Łój, M.
Madej, J.
Porzucek, S.
Zuchiewicz, W.

Powiązania:

https://bibliotekanauki.pl/articles/183924.pdf

Data publikacji:

2009

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

neotektonika
czasowe zmiany przyspieszenia siły ciężkości
Karpaty Zachodnie
Polska Południowa
temporal gravity changes
neotectonics
Western Carpathians
South Poland

Opis:

Multidisciplinary studies conducted along two geodynamic test transects across the Polish segment of the Western Carpathians, crossing the Orava Basin in the west and the Pieniny Klippen Belt and Magura Nappe along the Dunajec River valley in the east, included gravity and geodetic surveys as well as geological investigations. Gravity and geodetic surveys were carried out annually in years 2004-2006. Their results appear to suggest recent subsidence of the Orava Basin, particularly intensive in a Quaternary graben in the northern part of the area, confirming conclusions derived from geomorphic analyses. Data obtained for the Dunajec River transect do not show any particular differentiation among individual benchmarks, what can point to either minor uplift of the entire area, minimal differences between successive slices of the Magura Nappe and the Pieniny Klippen Belt, or both. Horizontal displacements of benchmarks, different for the western and eastern transects, towards the west and SW as well east and SE, respectively, can result from general uplift of the area comprised between these transects. On the other hand, the N to NNE-oriented vectors of recent horizontal motions, observed for stations located south of the Pieniny Klippen Belt, point to the ongoing NNE-directed push of the ALCAPA block.
Zintegrowane studia grawimetryczne, geodezyjne i geologiczno-geomorfologiczne przeprowadzono na dwóch profilach przecinających szereg jednostek środkowej części Karpat polskich, wykazujących zróżnicowane tendencje neotektoniczne: w poprzek Kotliny Orawskiej na zachodzie oraz wzdłuż beskidzkiego przełomu Dunajca na wschodzie. Pomiary grawimetryczne i geodezyjne wykonywano corocznie w okresie 2004--2006. Ich wyniki wskazują na współczesną subsydencję Kotliny Orawskiej, szczególnie intensywną w obrębie rowu Wróblówki. Dane uzyskane dla profilu Dunajca nie ujawniają większego zróżnicowania pomiędzy poszczególnymi punktami pomiarowymi, co może sugerować słabe wypiętrzanie całego obszaru i/lub minimalne różnice mobilności kolejnych łusek płaszczowiny magurskiej oraz pienińskiego pasa skałkowego. Przemieszczenia poziome reperów usytuowanych w obrębie Karpat zewnętrznych, a skierowane ku zachodowi i SW w profilu zachodnim oraz ku wschodowi i SE w profilu wschodnim, mogą odzwierciedlać wypiętrzanie obszaru ograniczonego profilami, tj. masywu Gorców. Natomiast skierowane ku północy i NNE wektory współczesnych ruchów poziomych dla stanowisk ulokowanych na południe od pienińskiego pasa skałkowego zdają się wskazywać na nadal aktywny nacisk bloku ALCAPA ku NNE.

Źródło:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2009, 35, 2; 217-247
0138-0974

Pojawia się w:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 72.

Tytuł:

Blueschists in the Cretaceous exotic conglomerates of the Klape Unit (Pieniny Klippen Belt, Western Carpathians): their genetic types and implications for source area
Łupki glaukofanowe w kredowych zlepieńcach egzotykowych jednostki klapskiej (pieniński pas skałkowy, Karpaty Zachodnie): ich typy genetyczne i implikacje dla obszaru źródłowego

Autorzy:

Ivan, P.
Sykora, M.
Demko, R.

Powiązania:

https://bibliotekanauki.pl/articles/183557.pdf

Data publikacji:

2006

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

Karpaty Zachodnie
alb
zlepieńce egzotykowe
łupki glaukofanowe
utwory wulkaniczne
geochemia
Western Carpathians
Albian
exotic conglomerates
blueschists
volcanics
geochemistry

Opis:

In the Klape Unit of the Pieniny Klippen Belt the Albian conglomerates with clasts of exotic carbonates, clastic sediments and also volcanic and plutonic rocks are relatively widespread. In the small area near the town Povażska Bystrica also scarce blueschist clasts of variegated petrographic types have been found. Three groups of starting rocks can be discerned for blueschists: pelagic sediments, metamorphic rocks (amphibolites, gneisses) and volcanic rocks. Based on immobile trace element (HFSE, REE) distribution two petrogenetic types of volcanic rocks have been identified: basalts with BABB signature and calc-alkaline basaltic andesites to rhyolites. Source of these rocks was probably a nappe stack located in the Carpathian interior and created in the Late Jurassic time as a result of subduction of the oceanic crust and adjacent volcanic arc and followed by collision during the Meliata Ocean closure
Albskie zlepieńce jednostki klapskiej pienińskiego pasa skałkowego zawierające egzotyki skał węglanowych, klastycznych, jak również wulkanicznych i plutonicznych są szeroko rozprzestrzenione. Na małym obszarze w okolicy Povażskiej Bystricy (Słowacja zachodnia) w kilku stanowiskach znaleziono rzadkie egzotyki zróżnicowanych petrograficznie łupków glaukofanowych. Wyróżniono trzy grupy pierwotnych utworów przekształconych w te łupki: osady pelagiczne, skały metamorficzne (amfibolity, gnejsy) i skały wulkaniczne. W oparciu o niestabilne pierwiastki śladowe (HFSE, REE) zidentyfikowano dwa typy petrogenetyczne skał wulkanicznych: bazalty o cechach bazaltów obszarów zaułkowych (BABB) oraz wapniowo-alkaliczne andezyty i ryolity bazaltowe. Obszarem źródłowym tych skał były prawdopodobnie spłaszczowinowane jednostki zlokalizowane w obrębie Karpat wewnętrznych, powstałe w późnej jurze jako rezultat subdukcji skorupy oceanicznej i utworzonego w związku z tym łuku wulkanicznego, w następstwie kolizji podczas zamykania się oceanu Meliaty

Źródło:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2006, 32, 1; 47-63
0138-0974

Pojawia się w:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 73.

Tytuł:

Where was the Magura Ocean?

Autorzy:

Oszczypko, N.
Ślączka, A.
Oszczypko-Clowes, M.
Olszewska, B.

Powiązania:

https://bibliotekanauki.pl/articles/139322.pdf

Data publikacji:

2015

Wydawca:

Polska Akademia Nauk. Czytelnia Czasopism PAN

Tematy:

Cenozoic
Outer Western Carpathians
palaeogeography
intrabasinal ridges
basin development
kenozoik
Zewnętrzne Karpaty Zachodnie
paleogeografia
grzbiet śródbasenowy
basen
rozwój

Opis:

In the Late Jurassic to Early Cretaceous palaeogeography of the Alpine Tethys the term Ocean is used for different parts of these sedimentary areas: eg. Ligurian – Piedmont and Penninic, Magura, Pieniny, Valais and Ceahlau-Severins oceans. The Magura Ocean occupied the more northern position in the Alpine-Carpathian arc. During the Late Cretaceous–Paleogene tectono-sedimentary evolution the Magura Ocean was transformed into several (Magura, Dukla, Silesian, sub-Silesian and Skole) basins and intrabasinal source area ridges now incorporated into the Outer Western Carpathians.

Źródło:

Acta Geologica Polonica; 2015, 65, 3; 319-344
0001-5709

Pojawia się w:

Acta Geologica Polonica

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 74.

Tytuł:

Rozwój badań utworów miocenu w Karpatach Zachodnich na obszarze Bielsko - Kraków
Development of research on Western Carpathian Miocene deposits in the Bielsko - Kraków area

Autorzy:

Moryc, W.

Powiązania:

https://bibliotekanauki.pl/articles/184012.pdf

Data publikacji:

2005

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

Karpaty Zachodnie
zapadlisko przedkarpackie
miocen
litostratygrafia
ewolucja basenu
tektogeneza
Western Carpathians
Carpathian Foredeep
Miocene
lithostratigraphy
basin evolution
tectogenesis

Opis:

W artykule przedstawiono, w ujęciu chronologicznym, omówienie poglądów dotyczących rozwoju litostratygraficznego utworów miocenu na obszarze polskich Karpat Zachodnich. Przedstawiono również wyniki badań utworów miocenu stwierdzonych na tym obszarze w szeregu nowych wierceń. W nawiązaniu do dotychczasowych badań i nowych obserwacji przedstawiono jednolitą korelację utworów miocenu, ze szczególnym uwzględnieniem osadów dolnomioceńskich. Określono występowanie i rozprzestrzenienie wyróżnionych jednostek litostratygraficznych oraz przedstawiono ewolucję basenu mioceńskiego i jego tektogenezę. Osady mioceńskie na obszarze polskich Karpat Zachodnich tworzą zespół utworów o sumarycznej miąższości dochodzącej do około 3000 metrów. Prawie połowę tej miąższości zajmują osady dolnego miocenu. W miarę nasuwania się ku północy górotworu karpackiego, następowało przesuwanie się mioceńskiego zbiornika i wkraczanie kolejno coraz to młodszych osadów. W utworach dolnego miocenu wyróżniono formacje z Zawoi, z Suchej, ze Stryszawy, a w dolnym badenie - formacje z Jachówki, dębowiecką i skawińską
The paper presents chronologically arranged discussion of existing views on the lithostratigraphic development of the Western Carpathian Miocene deposits as well as data from old and new boreholes in the studied area. The present author suggests the uniform stratigraphic division of the Miocene (especially Lower Miocene) deposits based on existing results and new findings. He also presents the occurrence and extent of distinguished lithostratigraphic units as well as the evolution of the Miocene basin and its tectogenesis. Miocene deposits in the Polish part of the Western Carpathians consist of thick deposit up to about 3000 meters. Almost half of these are represented by Lower Miocene deposits. The Miocene basin was moved northwards and younger deposits originated during folding processes of the Carpathian orogen. Several lithostratigraphical units were distinguished: Zawoja, Sucha and Stryszawa formations of the Lower Miocene deposits and Jachówki, Dębowiec and Skawina formations of the Lower Badenian one

Źródło:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2005, 31, 1; 5-73
0138-0974

Pojawia się w:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 75.

Tytuł:

K-Ar dating of bentonite diagenesis in accretionary-wedge turbidites : case study from Western Outer Carpathians

Autorzy:

Świerczewska, A.
Paul, Z.
Banaś, M.
Tokarski, A. K.

Powiązania:

https://bibliotekanauki.pl/articles/191676.pdf

Data publikacji:

2015

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

Bentonites
illite-smectite
K-Ar dating
accretionary-wedge turbidites
Western Outer Carpathians

Opis:

Sixteen bentonite layers of Eocene–Oligocene age were sampled at thirteen sites in accretionary-wedge turbidite sequences, in the three innermost nappes of the Western Outer Carpathians. K-Ar dating was carried out for five of these layers to obtain the maximum burial ages. All of the ages obtained are older than the stratigraphic ages of the host strata. This relationship is due to significant contamination of the bentonites with non-authigenic minerals. This contamination resulted from rapid sedimentation during synsedimentary folding, which is a common feature in accretionary wedges. It follows that the K-Ar dating of bentonite layers in the turbidite sequences of accretionary wedges should be largely restricted to the very distal facies of turbidites or to pelitic intercalations within the turbidites.

Źródło:

Annales Societatis Geologorum Poloniae; 2015, 85, 1; 177-185
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Tytuł:

Rola wyróżników i wyznaczników krajobrazu przyrodniczego i kulturowego w określeniu wyspowego charakteru Beskidu Małego
The role of landmarks and determinants of a natural and cultural landscape in defining the island character of the Little Beskids

Autorzy:

Łach, J.

Powiązania:

https://bibliotekanauki.pl/articles/88252.pdf

Data publikacji:

2016

Wydawca:

Polskie Towarzystwo Geograficzne

Tematy:

Karpaty Zachodnie
Beskid Mały
wyspiarskość
fizjonomia krajobrazu
góralszczyzna
polaniarstwo
Western Carpathians
Little Beskids
insularity
landscape physiognomy
highland culture
pastoralism

Opis:

Badania na potrzeby artykułu dotyczyły określenia wyspowego charakteru Beskidu Małego w stosunku do otaczającego go Beskidu Śląskiego, Beskidu Makowskiego, Kotliny Żywieckiej oraz Pogórza Śląskiego. W tym celu sięgnięto do metody wyróżników/wyznaczników krajobrazu na płaszczyźnie geograficznej oraz etnograficznej, badając jego izolację przestrzenną i kulturową. Z analizy elementów przyrodniczych za szczególny wyróżnik wyspowości Beskidu Małego wybrano rzeźbę oraz dominujący typ pokrycia terenu, natomiast z elementów etnograficznych za unikatowy wyróżnik przyjęto konstrukcyjny typ budowli polaniarskiej oraz przynależność etniczno-kulturową mieszkańców regionu. Zdefiniowane w artykule inne wyróżniki krajobrazowe stanowiące często pojedyncze, niewielkie płaty krajobrazowe, posiadające historyczne oraz geograficzne powiązania z regionem, pozwoliły z powyższymi wyróżnikami określić Beskid Mały jako krajobrazową wyspę górską Zewnętrznych Karpat Zachodnich.
The research for the needs of the article referred to the definition of island character of the Little Beskids in relation to surrounding Silesian Beskids, Makowski Beskids, Żywiec Basin and Silesian Foothills. To realize this goal, the method of landmarks and determiners of landscape was used on geographical and ethnographical plane examining its spatial and cultural isolation. From the analysis of the natural elements, terrain and dominant type of the land cover were chosen as a specific landmark of the island character. From ethnographic elements, structural type of pastoral buildings and ethno-cultural affiliation of the inhabitants of the Little Beskids were used as unique landmark. Other landscape landmarks defined in the article posing often single, small landscape patch with historical and geographical connections to the region allowed in the above determine the Little Beskids as a landscape mountain island in the Outer Western Carpathians.

Źródło:

Prace Komisji Krajobrazu Kulturowego; 2016, 33; 39-52
1896-1460
2391-5293

Pojawia się w:

Prace Komisji Krajobrazu Kulturowego

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 77.

Tytuł:

Tescheniceras gen. nov. (Ammonoidea) and the definition of the Valanginian/Hauterivian boundary in Butkov Quarry (Central Western Carpathians, Slovakia)

Autorzy:

Vašíček, Zdeněk

Powiązania:

https://bibliotekanauki.pl/articles/1835578.pdf

Data publikacji:

2020

Wydawca:

Polska Akademia Nauk. Czytelnia Czasopism PAN

Tematy:

Tescheniceras gen. nov.
Manín Unit
valanginian boundary
hauterivian boundary
taxonomy
Western Carpathians
jednostka Manín
Walanżyn
hoteryw
taksonomia
Karpaty Zachodnie

Opis:

Jurassic and Lower Cretaceous successions of the Manín Unit of the Central Western Carpathians are exposed in Butkov Quarry in the Middle Váh Region, Slovakia. A significant part of the macrofauna belonging to neocomitid ammonites, formerly classified under the genus Teschenites Thieuloy, 1971, occurs in deposits spanning the Valanginian/Hauterivian boundary. The original definition of Teschenites was accompanied by uncertainties in the taxonomic and stratigraphic position of its original type species, i.e., Hoplites neocomien-siformis Uhlig, 1902. The present contribution focuses on and provides a possible taxonomic solution by es-tablishing the new genus Tescheniceras. In Butkov Quarry, the new genus includes five species. Tescheniceras flucticulum (Thieuloy, 1977), the type species, is the most abundant. Tescheniceras callidiscum (Thieuloy, 1971), the subzonal species for the uppermost Valanginian (Thieuloy 1971b), occurs only sporadically. Because Acanthodiscus radiatus (Bruguiére, 1789), the index species for the basal Hauterivian (radiatus Zone) in the international ammonite zonation, does not occur in the locality, the basal Hauterivian is indicated by the first appearance of the genus Spitidiscus Kilian, 1910.

Źródło:

Acta Geologica Polonica; 2020, 70, 4; 569-584
0001-5709

Pojawia się w:

Acta Geologica Polonica

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 78.

Tytuł:

New record of macrofungi for the mycobiota of the Cieszyn municipality (Polish Western Carpathians) including new species to Poland

Autorzy:

Chachuła, Piotr
Fiedor, Marek
Rutkowski, Ryszard
Dorda, Aleksander

Powiązania:

https://bibliotekanauki.pl/articles/11543321.pdf

Data publikacji:

2020

Wydawca:

Polskie Towarzystwo Botaniczne

Tematy:

mycological research
Ascomycota
Basidiomycota
hypogeous fungi
mycorrhizal fungi
parasitic fungi
saprotrophic fungi
mycobiota
Cieszyn commune
Western Carpathians Mountains
Polska

Opis:

In this paper, we present the results of mycological research carried out between 2015 and 2018 in the Cieszyn township, in the Silesian Foothills (Outer Western Carpathians). The list of 417 species of macrofungi from the Cieszyn area reported in our previous study, has been expanded further by the addition of 37 taxa found in the current study. Among these, the following deserve special attention: fungi that are new to Poland’s mycobiota (six species: Bryoscyphus dicrani, Discina martinii, Elaphomyces aculeatus, Tuber brumale, T. foetidum, and Russula cerea), taxa subject to legal protection (four species: Disciotis venosa, Grifola frondosa, Mitrophora semilibera, and Sparassis brevipes), as well as fungi that are rare in Poland, included in national or regional red lists, and in the registers of rare and endangered species (24 species including Amanita echinocephala, Arrhenia retiruga, A. spathulata, Catinella olivacea, Elaphomyces maculatus, Hygrophorus discoxanthus, Ophiocordyceps entomorrhiza, Pluteus diettrichii, Tuber aestivum, and T. fulgens). This paper presents the distribution and location of 32 species of fungi along with a short description and illustration of the macro- and micromorphological features of select species and their habitats.

Źródło:

Acta Mycologica; 2020, 55, 1; 5511
0001-625X
2353-074X

Pojawia się w:

Acta Mycologica

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 79.

Tytuł:

Lower Jurassic to lower Middle Jurassic succession at Kopy Sołtysie and Płaczliwa Skała in the eastern Tatra Mts (Western Carpathians) of Poland and Slovakia: stratigraphy, facies and ammonites

Autorzy:

Iwańczuk, J.
Iwanow, A.
Wierzbowski, A.

Powiązania:

https://bibliotekanauki.pl/articles/2061015.pdf

Data publikacji:

2013

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

stratigraphy
Middle Jurassic
ammonites
microfacies
correlation
Tatra Mts.
Western Carpathians
stratygrafia
jura środkowa
amonity
mikrofacja
korelacja
Tatry
Karpaty Zachodnie

Opis:

The Lower Jurassic and the lower part of the Middle Jurassic deposits corresponding to the Sołtysia Marlstone Formation of the Lower Subtatric (Krížna) nappe in the Kopy Sołtysie mountain range of the High Tatra Mts and the Płaczliwa Skała (= Ždziarska Vidla) mountain of the Belianske Tatra Mts in the eastern part of the Tatra Mts in Poland and Slovakia are described. The work concentrates both on their lithological and facies development as well as their ammonite faunal content and their chronostratigraphy. These are basinal deposits which show the dominant facies of the fleckenkalk-fleckenmergel type and reveal the succession of several palaeontological microfacies types from the spiculite microfacies (Sinemurian–Lower Pliensbachian, but locally also in the Bajocian), up to the radiolarian microfacies (Upper Pliensbachian and Toarcian, Bajocian–Bathonian), and locally the Bositra (filament) microfacies (Bajocian–Bathonian). In addition, there appear intercalations of detrital deposits – both bioclastic limestones and breccias – formed by downslope transport from elevated areas (junction of the Sinemurian and Pliensbachian, Upper Toarcian, and Bajocian). The uppermost Toarcian – lowermost Bajocian interval is represented by marly-shaly deposits with a marked admixture of siliciclastic material. The deposits are correlated with the coeval deposits of the Lower Subtatric nappe of the western part of the Tatra Mts (the Bobrowiec unit), as well as with the autochthonous-parachthonous Hightatric units, but also with those of the Czorsztyn and Niedzica successions of the Pieniny Klippen Belt, in Poland. The character of the deposits in the sequences, and their biostratigraphical analysis, show that sedimentation during the Early Jurassic, and up to the Late Bajocian, was controlled by rifting phases which were active at the junction of the Sinemurian and Pliensbachian (Zliechov Phase), during the Late Pliensbachian and Toarcian (Devín Phase), and during the Bajocian (Krasín Phase). The onset of pelagic sedimentation overlying the rift strata took place during the latest Bajocian. Selected ammonite taxa are illustrated and discussed.

Źródło:

Volumina Jurassica; 2013, 11, 1; 19--58
1896-7876
1731-3708

Pojawia się w:

Volumina Jurassica

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 80.

Tytuł:

Obwodnice drogowe w tradycyjnym krajobrazie wiejskim okolic Tylicza
Ring roads in the traditoinal rural landscape of the environs of Tylicz place

Autorzy:

Sroczyński, Wiesław

Powiązania:

https://bibliotekanauki.pl/articles/88212.pdf

Data publikacji:

2009

Wydawca:

Polskie Towarzystwo Geograficzne

Tematy:

obwodnica drogowa
ochrona tradycyjnego krajobrazu wiejskiego
Łemkowszczyzna
polskie Karpaty Zachodnie
bypass
protection of the traditional rural landscape
Polish Western Carpathians

Opis:

Przedstawiono konflikty krajobrazowe, przyrodnicze i przestrzenne związane z planami rozbudowy drogi krajowej nr 75 Krzyżówka-Tylicz do granicy państwa. Krajobraz jest typowy dla Beskidu Niskiego, z dużym udziałem terenów otwartych, głównie łąk porolnych i zarośli podlegających regeneracji po wysiedleniach w 1947 r. Uzasadnia to włączenie omawianego obszaru w 2007 r. do sieci Natura 2000. Zabytki kultury materialnej koncentrują się przy istniejącej drodze, pośród zabudowy. Potencjalne warianty planowanego przedsięwzięcia to: rozbudowa drogi po istniejącym śladzie, zaprojektowanie obwodnic dla poszczególnych miejscowości, ponad linią zabudowy, skierowanie drogi krajowej nowym korytarzem poprzez partie grzbietowe z poprzecznymi dojazdami do miejscowości. Wszystkie wymienione warianty kolidują z postulatem zachowania trwałości tradycyjnych krajobrazów wiejskich.
In the paper, landscape, nature and space conflicts connected with plans of a trunk road no. 75 Krzyzowka-Tylicz-border development are presented. Places situated near this route are distinguished by location value in the observational valley segments. The landscape is typical for the Low Beskids, with great participation of open spaces, mainly post-arable meadows (c.a. 49%). This is a secondary but harmonious landscape, on the land which was subjected to displace after World War II (1947). Boundaries between forest and non-forest communities are unsteady, with tendency to enlarge an area of wooded land. That mosaic of semi-natural agriculture and forest grounds is a valuable natural habitat. This was a good reason to include a discussed region to the European Ecological Natura 2000 Network in 2007. Monuments are concentrated near the existing road, among the buildings. Potential variants of planned project are connected with: (1) road development after existing track, (2) making a project of ring roads for particular places, above line of building development, (3) directing a trunk road by a new corridor through the mountain ridge parts, with lateral accesses to the places. All presented variants collide with postulate of conservation of traditional rural landscape durability. Variant connects with existing track should be evaluated as destructive for local „landscape interiors” and excessively arduous for people. Its advantages are protection of semi-natural, extensive arable land and distant observational exposures (panoramas watch from hills and ridges). Selection of that option does not guarantee a solution of communication problems in the longer perspective. Variants with ring roads by-passing the building lands (in different combinations) can ensure a protection of country profile in the local scale and keep social bonds. Worsening of landscape beauty in the general scale is an unavoidable cost. It refers to the most multi-directional observational panoramas with surrounding mountain ranges. Selection of that option indicates a greater intervention into seminatural systems (in the acceptable boundaries). Possibility of action division is a significant advantage of this variant selection. Searching of new corridors for trunk road, some distance from places, does not predict a success, because of requirements of forest, habitat and species from Natura 2000 network protection. Intervention into landscape and nature systems can be in this situation the most meaningful. A possible tunnel building should be excluded on this area because of mineral water threat.

Źródło:

Prace Komisji Krajobrazu Kulturowego; 2009, 12; 158-165
1896-1460
2391-5293

Pojawia się w:

Prace Komisji Krajobrazu Kulturowego

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 81.

Tytuł:

Wykształcenie facjalne warstw krośnieńskich w oknie tektonicznym Mszany Dolnej (polskie Karpaty Zachodnie)
Facial development of the Krosno Beds in the Mszana Dolna tectonic window (Polish Western Carpathians)

Autorzy:

Stadnik, R.

Powiązania:

https://bibliotekanauki.pl/articles/183958.pdf

Data publikacji:

2007

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

Karpaty Zachodnie
okno tektoniczne Mszany Dolnej
warstwy krośnieńskie
oligocen
facje
Oligocene
Western Carpathians
Mszana Dolna tectonic window
Krosno Beds
facies

Opis:

Przedmiotem opracowania są warstwy krośnieńskie odsłaniające się w oknie tektonicznym Mszany Dolnej w obrębie jednostki dukielskiej. Utwory te wykształcone są głównie w litofacji piaskowców, piaskowców z mułowcami, mułowców z piaskowcami oraz mułowców. Podczas analizy sprofilowanych odsłonięć brano przede wszystkim pod uwagę następujące cechy: wykształcenie litofacjalne, miąższości ławic, procentowy udział piaskowców w stosunku do skał zbudowanych z frakcji drobniejszych, wysortowanie materiału okruchowego, a także rodzaj powierzchni spągowych i stropowych ławic oraz obecność sekwencji negatywnych i pozytywnych w profilu. W konsekwencji rozpoznano środowisko sedymentacji tych utworów. Wykazano, że warstwy krośnieńskie powstawały w obrębie głębokomorskich stożków, w strefie stożka zewnętrznego, w subśrodowisku lobów depozycyjnych, obrzeżenia lobu i obrzeżenia stożka. Na podstawie próbek mikrofaunistycznych oznaczono wiek warstw krośnieńskich na oligocen (zona NP24). Pomierzone kierunki paleotransportu wskazują, że transport materiału okruchowego odbywał się z kierunku południowo-zachodniego na północny wschód.
The present author studied the Krosno beds outcropped in the Mszana Dolna tectonic window within the Dukla Unit. These deposits are mainly developed as sandstones, sandstones with mudstones, mudstones with sandstones and mudstones. The following features: lithofacial development, thickness of layers, the percentage of sandstones in relation with the fine-grained rocks, clastic sediments sorting as well the character of bottom and top surfaces of layers and the presence of the positive and negative sequences in a profile were taken into account for the analysis of the geological profiled outcrops. Such sedimentological features of the Krosno beds indicate their depositional environment connected with the deep-sea fans, in the area of the lower fan, in the subenvironment of the depositional lobes, the lobe fringe and the fan fringe. Based on the microfossils the age of the Krosno beds has been indicated as Oligocene (zona NP24). The measured directions of the palaeotransport show that the distribution of the clastic material took place from the SW to the NE.

Źródło:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2007, 33, 4; 375-393
0138-0974

Pojawia się w:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 82.

Tytuł:

Próba przestrzennej analizy rozkładu oporności na podstawie interpretacji sondowań magnetotellurycznych w rejonie Lachowice - Zawoja w polskich Karpatach Zachodnich
An attempt of spacial analysis of resistivity distribution based on interpretation of magnetotelluric soundings in the Lachowice - Zawoja area, Polish Western Carpathians

Autorzy:

Klityński, W.
Stefaniuk, M.

Powiązania:

https://bibliotekanauki.pl/articles/183831.pdf

Data publikacji:

2007

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

Karpaty Zachodnie
sondowania magnetotelluryczne
interpretacja 3D
modelowania 3D
Western Carpathians
magnetotelluric sounding
3D interpretation
3D modelling

Opis:

W prezentowanej pracy przedstawiono próbę konstrukcji modelu 3D rozkładu oporności wykonaną dla obszaru Lachowice - Zawoja w polskich Karpatach Zachodnich. Rejon ten przecinają odcinki czterech regionalnych profili magnetotellurycznych. Znaczne zagęszczenie sondowań w tym obszarze pozwala na podjęcie przestrzennej analizy rozkładu oporności. Wyniki inwersji 1D, według algorytmu Occama, posłużyły do opracowania map oporności w cięciach poziomych, ilustrujących przestrzenne zróżnicowanie tego parametru. Do konstrukcji wstępnego modelu 3D wykorzystano wyniki interpretacji 1D i 2D. Wstępny model trójwymiarowy weryfikowany był i poprawiany poprzez wielokrotnie powtarzane modelowanie proste 3D. Podkreślić należy, że jest to pierwsza w Polsce próba wykorzystania modelowania 3D do analizy wyników sondowań magnetotellurycznych.
An attempt of construction of 3D model of resistivity distribution made for Lachowice-Zawoja area in western part of Polish Carpathians is presented in the paper. The study area is cut by sections of four regional magnetotelluric profiles. Significant density of MT soundings in the area allows to undertake of the spatial analysis of resistivity distribution. Results of 1D Occam inversion were used to elaborate resistivity maps on selected depth levels that illustrates spatial resistivity differentiation. The entrance 3D resistivity model was made based on results of 1D and 2D sounding interpretation. The starting spatial model was verified and corrected by repeatedly recurred forward 3D modelling. It should be stated that this is the first attempt of use of 3D modelling for analysis of magnetotelluric soundings in Poland.

Źródło:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2007, 33, 4/1; 127-142
0138-0974

Pojawia się w:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 83.

Tytuł:

Mineralizacja gipsowa w warstwach hieroglifowych antykliny Jankowej (Zachodnie Karpaty Zewnętrzne) – wstępne wyniki badań
Gypsum mineralization in hieroglyphic beds of the Jankowa anticline – preliminary research results (Outer Western Carpathians)

Autorzy:

Gąsienica, Aleksander
Kozłowski, Adam
Drzewicki, Wojciech

Powiązania:

https://bibliotekanauki.pl/articles/20228848.pdf

Data publikacji:

2023

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

gips
mineralizacja siarczanowa
antyklina Jankowa
jednostka śląska
Zewnętrzne Karpaty Zachodnie
gypsum
sulfate mineralization
Jankowa anticline
Silesian Unit
Outer Western Carpathians

Opis:

Sulfate mineralization occurs in almost all lithostratigraphic beds of the Carpathians and has been described for at least the last century. While carrying out cartographic studies near Bobowa, a new site of gypsum mineralization was discovered within the hieroglyphic beds of the Jankowa anticline. The gypsum crystals found there reach up to several centimetres in length and, so far, no similar ones have been described in the Carpathian flysch deposits. Gypsum from Jankowa occurs in the form of intergrowth and twinnings, rosettes and larkspurs, and vein fillings.

Źródło:

Przegląd Geologiczny; 2023, 71, 4; 169-173
0033-2151

Pojawia się w:

Przegląd Geologiczny

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 84.

Tytuł:

The tectonic setting and origin of the Smilno tectonic window (Eastern Slovakia)
Założenia tektoniczne i geneza okna tektonicznego Smilna (wschodnia Słowacja)

Autorzy:

Ryłko, W.
Tomaś, A.

Powiązania:

https://bibliotekanauki.pl/articles/2062510.pdf

Data publikacji:

2012

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Smilno tectonic window
Magura
Grybów and Dukla units
Western Carpathians
okno tektoniczne Smilna
jednostka magurska
Karpaty Zachodnie
jednostka grybowska
jednostka dukielska

Opis:

The Smilno tectonic window is located in eastern Slovakia between Smilno in the west and Nižný Mirošov in the east. Geologically, the Smilno tectonic window occurs in the Magura Unit, within the Racza Subunit. In this area, deposits of the Grybów and Dukla units crop out from under the Magura Unit rocks and occur at the surface. The Dukla Unit section is represented by the Submenilite Formation occurring in the northern part of the window. The upper Grybów Unit is represented by the Menilite Formation and the Krosno Beds. The Smilno window developed as a result of a multi-stage formation of flysch masses in this region. In the earliest stage, flysch masses were displaced over the Makovice Ridge from the south into the graben. The graben was filled mostly with deposits of the Silesian and Dukla units, overlain by the Grybów and Magura units. In the next stage, there was a restructuring of the Makovice Ridge, which extended into the overlying deposits of the Silesian and Dukla units. During the later stage, tectonic deformation spread out into the Grybów and Magura units. Not only discontinuous tectonic deformation, but also the beginnings of folding processes, developed as a result of SW-oriented stress, is observed within them. In the next stage, the SW-oriented stress plays a significant role. It resulted in a shift of the Grybów and Magura units and the top part of the Dukla Unit in relation to the Dukla and Silesian units. The last stage included primarily a shortening and thrusting of the Grybów and Magura units and the top portion of the Dukla Unit. Due to this process, the Magura Unit broke up, and the Grybów and Dukla units, today present in the Smilno window, pierced up to the surface along discontinuity planes. In each case described, the occurrence of a tectonic window within flysch deposits was associated with the presence of a resisting element in the consolidated basement of the Carpathians to the south of the window zone; in the case of the Smilno window, it was the Makovice Ridge.
Tektoniczne okno Smilna położone jest na obszarze wschodniej Słowacji, w obrębie jednostki magurskiej. W obrębie okna Smilna mamy do czynienia z profilami dwóch jednostek, jednostki dukielskiej i jednostki grybowskiej. Okno Smilna uformowało się w rowie podłoża pomiędzy grzbietem makowickim na południu a regionalnym skłonem podłoża na północy. Powstało ono w wyniku wieloetapowego formowania się mas fliszowych. W każdym opisanym przypadku pojawienie się okna tektonicznego w obrębie mas fliszowych związane było z wystąpieniem elementu oporowego w skonsolidowanym podłożu Karpat na południe od strefy okiennej. Element ten był przeszkodą dla ruchu mas fliszowych ku północy, wyhamowywał go i w wyniku tego powstawała składowa pionowa sił powodująca wypiętrzenie mas fliszowych z głębi na powierzchnię. W przypadku okna Smilna był to grzbiet makowicki.

Źródło:

Biuletyn Państwowego Instytutu Geologicznego; 2012, 449; 185--193
0867-6143

Pojawia się w:

Biuletyn Państwowego Instytutu Geologicznego

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 85.

Tytuł:

Modification of life history and morphometric traits of montane species as an expression of adaptive abilities to different climatic conditions - a case study of Petasites kablikianus Tausch ex Bercht. (the Babia Gora Mt, Western Carpathians, Poland)

Autorzy:

Uzieblo, A.K.

Powiązania:

https://bibliotekanauki.pl/articles/58757.pdf

Data publikacji:

2015

Wydawca:

Polskie Towarzystwo Botaniczne

Tematy:

Petasites kablikianus
Compositae
modification
life history
morphometric analysis
montane species
adaptive ability
climate condition
Babia Gora Massif
Western Carpathians Mountains
Polska

Opis:

Detailed data on the response of plants to different climatic conditions could gain insight into the early impacts of climate change upon functioning ecosystems especially alpine ones, the most specialized. Petasites kablikianus (Asteraceae) is a species with montane and disjunctive distribution range, and it is one of the best objects to such investigations. In Polish high mountains, it is represented the best on the northern slopes of the Babia Góra massif (the Babiogórski National Park) and it occurs in two, independent zones: subalpine (landslides, rock rubbles) and lower montane zone (gravels on stream banks). The climatic differences between these two zones result in a morphological differentiation of specimens but mainly in differences in the dynamics of the life history of both populations. Detailed phenological observations and biometrical measurements were made on five plots on both gynodynamic and androdynamic shoots in their natural environment and after transplantation. The most important result is a fact that the subalpine population is completely phenologically isolated. Moreover the differences in the dates of beginning vegetation and in the duration and dynamics of particular stages of development and in morphological structure of individuals between the upper and lower populations were also stated. The results show that the adaptability of the species present a great potential to respond to the possible effects of global warming by modifying the life history and extending of distribution range for low-lying areas.

Źródło:

Acta Societatis Botanicorum Poloniae; 2015, 84, 4
0001-6977
2083-9480

Pojawia się w:

Acta Societatis Botanicorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 86.

Tytuł:

Analysis of selected problems encountered while testing natural gas-condensate fields in the Western Carpathians

Autorzy:

Rybicki, Cz.
Dubiel, S.
Blicharski, J.

Powiązania:

https://bibliotekanauki.pl/articles/298763.pdf

Data publikacji:

2015

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

oil prospecting
Western Carpathians
gas-bearing Devonian strata
natural gas-condensate field in Stryszawa
testing technology
thermodynamic conditions of gas condensation

Opis:

The potential change of natural gas composition in the near-wel lbore zone creates a big problem with the selection of appropriate initial value of counterpressure exerted by the displacement fluid on reservoir during the test, and also with the interpretation of the reservoir and production tests results. The analysis of the industrial data reveals that the effect of condensate production in the near-wellbore zone could take place while using too high counterpres-sure during DST tests, as a consequence of using a relatively high column of water displacement fluid in the DST column, i.e. about 2500 m. This thesis can be confirmed after further detailed theoretical analysis of the occurring thermodynamic conditions. The paper addresses technological and interpretation problems encountered during drill stem tests (DST) of gas-bearing Devonian strata, on the example of the Stryszawa field in the Western Carpathians. Special attention was paid to the possible changes of gas compo sition during flow tests and the cases of gas condensation of heavier fractions during build-up tests. Attempts were made at explaining sudden drops of pressure at the build-up stage along with the thermodynamic conditions responsible for this effect. The authors explained the necessity of using an appropriate Ful-Flo sampler in the DST set for collecting gas samples at any time of the test, and devices for continuous measurement of temperature. The use of new types of drill stem testers and appropriate interpretation methods, which would account for a detailed analysis of technological and reservoir conditions allows for more efficient oil prospecting and deciding about enhancement methods in hydrocarbon production. The analysis of thermodynamic conditions on the bottom of the wellbore allow s for selecting proper counterpressure values in view of the condensation of heavier gas fractions in the near wellbore rocks. The analysis of conditions in which heavier gas fractions undergo condensation is approximate and general because the gas samples were collected at the outlet of the DST string (in surface conditions), without a Ful-Flo sampler and without temperature measurements.

Źródło:

AGH Drilling, Oil, Gas; 2015, 32, 3; 575-580
2299-4157
2300-7052

Pojawia się w:

AGH Drilling, Oil, Gas

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 87.

Tytuł:

Utwory formacji wierzowskiej na tle wczesnokredowych warunków sedymentacji w zachodniej części basenu protośląskiego (Morawy, Republika Czeska)
Verovice Formation deposits during Early Cretaceous sedimentological regimes in the western part of the proto-Silesian Basin (Moravia, the Czech Republic)

Autorzy:

Strzeboński, P.
Golonka, J.
Waśkowska, A.
Krobicki, M.
Słomka, T.
Skupien, P.
Vasicek, Z.

Powiązania:

https://bibliotekanauki.pl/articles/183429.pdf

Data publikacji:

2009

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

Zewnętrzne Karpaty Zachodnie
formacja wierzowska
kreda wczesna
basen protośląski
Czechy
Outer Western Carpathians
Verovice Formation
Early Cretaceous
proto-Silesian Basin
Czech Republic

Opis:

Sedimentological development of the Verovice Formation (Czech Moravia) is presented, according to Early Cretaceous geotectonic-eustatic changes in the proto-Silesian Basin. Those processes were a consequence of a gradual rebuilding the architecture of the Alpine-Carpathian realm. The geological events well correspond with the global sequence stratigraphy.

Źródło:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2009, 35, 2/1; 31-38
0138-0974

Pojawia się w:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 88.

Tytuł:

Budowa geologiczna doliny Białego Dunajca
Geology of the Biały Dunajec Valley (Podhale region, S Poland)

Autorzy:

Mastella, L.
Ludwiniak, M.
Klimkiewicz, D.

Powiązania:

https://bibliotekanauki.pl/articles/2074964.pdf

Data publikacji:

2012

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

zachodnie Karpaty centralne
synklinorium podhalańskie
strefa uskokowa Białego Dunajca
sieć uskoków
Central Western Carpathians
Podhale Synclinorium
Biały Dunajec fault zone
fault network

Opis:

The Biały Dunajec Valley is one of the large, meridionally oriented valleys cutting the Podhale Synclinorium. The tectonic origin of this valley has been suggested since the beginning of the 20th century. A large fault zone with an azimuth of about 20° has been recognized here. This zone extends to the north and cuts the Pieniny Klippen Belt, which is significantly lowered in its eastern side. The southern part of the Biały Dunajec fault zone (SBD) extends probably into the Tatra Massif (into the Mała Łąka Valley area and far to the south into the border of the Koszysta elevation and the Goryczkowa depression). The majority of faults constituting the SBD were formed during the initial phase as strike-slip faults; they were reactivated later as dip-slip faults with a prevailing dip-slip, mainly normal component. As a whole, the SBD is a scissor-like fault: in the northern part, near the Szaflary village, downfaulted is its eastern block, whereas in the southern part - its western block.

Źródło:

Przegląd Geologiczny; 2012, 60, 9; 496--505
0033-2151

Pojawia się w:

Przegląd Geologiczny

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 89.

Tytuł:

Miocene transpression effects at the boundary of Central Carpathian Paleogene Basin and Pieniny Klippen Belt - examples from Polish-Slovakian borderland

Autorzy:

Ludwiniak, M.

Powiązania:

https://bibliotekanauki.pl/articles/184548.pdf

Data publikacji:

2018

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

structural geology
tectonics
Western Central Carpathians
Podhale basin
Spišska Magura
faults
folds
joints
calcite veins

Opis:

A geological structural study has been conducted along the tectonic contact zone of the Central Carpathian Paleogene Basin (CCPB) and Pieniny Klippen Belt (PKB) in the eastern Podhale and western Spišska Magura areas. It concerned mostly the Central Carpathian Paleogene flysch strata and, to a lesser degree, the Upper Cretaceous rocks of the PKB. Tectonic deformation structures genetically related to the important tectonic boundary in question occur within a c. 1.5–2 km-wide strip of the Paleogene flysch rocks adjacent from the south to the PKB. Two parallel structural domains have been distinguished within this strip: the contact zone proper in the north and the peri-Pieniny monocline in the south. Most of the minor faults documented in the Paleogene flysch bear a record of dextral motion parallel to the contact zone. Some dextral-reverse oblique slip faults of NE-SW and W-E trends have also been recognized. Discrepancies in the orientation and sense of movement on strike-slip faults in the Paleogene flysch rocks and those in marlstones of the “klippen envelope” of the PKB were encountered. They probably reflect differences in the structural history of both the adjacent rock complexes, as the Upper Cretaceous deposits of the PKB must have experienced more deformation events and, in general, were affected by much more intense strain than those of the CCPB. Contractional structures, such as south-vergent reverse faults and recumbent folds which point to ca N-S tectonic shortening, have also been found in the Paleogene rocks. The entirety of the structural features found in the CCPB is characteristic of a transpressional regime. The regionally consistent coexistence of structures resulting from strike-slip movements and tectonic shortening, as well as features pointing directly to a transpressional regime, prove the transpressional dextral nature of the contact between the CCPB and PKB.

Źródło:

Geology, Geophysics and Environment; 2018, 44, 1; 91-100
2299-8004
2353-0790

Pojawia się w:

Geology, Geophysics and Environment

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 90.

Tytuł:

Granice złóż gazu ziemnego Lachowice i Stryszawa w świetle testów rurowym próbnikiem złoża
Boundaries of the Lachowice and Stryszawa gas deposits in view of DST tests

Autorzy:

Dubiel, S.
Rzyczniak, M.
Solecki, M. L.
Maruta, M.

Powiązania:

https://bibliotekanauki.pl/articles/2075365.pdf

Data publikacji:

2015

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Karpaty Zachodnie
DST
metoda log-log
złoża gazu Stryszawa i Lachowice
Western Carpathians
Drill Stem Test
log-log method
Stryszawa and
Lachowice gas deposits

Opis:

Identification of hydrocarbon accumulation boundaries within an oil field area is an important factor for making decisions whether or not to drill out and develop the field, or to give up extraction in some parts of the areas. As an example, two gas/condensate fields in the Devonian strata of the Western Carpathians are presented in this paper. These deposits were found at various depths in the Miocene basement in two separate tectonic blocks. Boundaries of the Stryszawa field were identified with the traditional Horner method and with the modern log-log method on the basis of industrial data obtained with DST and production tests. Based on the analysis of the drilling-up and testing methods used in the L-4 well in the Devonian strata of the Lachowice field the authors formulated the causes of considerably lower inflow of reservoir fluid to the tester during four DST tests, and the inability to determine boundaries of this part of the deposit.

Źródło:

Przegląd Geologiczny; 2015, 63, 1; 60--66
0033-2151

Pojawia się w:

Przegląd Geologiczny

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 91.

Tytuł:

Lithostratigraphy and biostratigraphy of the Upper Albian-Lower/Middle Eocene flysch deposits in the Bystrica and Rača subunits of the Magura Nappe (Beskid Wyspowy and Gorce Ranges; Poland)
Lito- i biostratygrafia utworów fliszowych górnego albu-dolnego/środkowego eocenu w jednostce bystrzyckiej i raczańskiej płaszczowiny magurskiej w Beskidzie Wyspowym i Gorcach (Zachodnie Karpaty fliszowe)

Autorzy:

Oszczypko, N.
Malata, E.
Bąk, K.
Kędzierski, M.
Oszczypko-Clowes, M.

Powiązania:

https://bibliotekanauki.pl/articles/191454.pdf

Data publikacji:

2005

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

lithostratigraphy
biostratigraphy
deep-water agglutinated foraminifera
calcareous nannoplankton
Early Cretaceous–Palaeogene
Magura Nappe
Western Flysch Carpathians

Opis:

LithostratigraphyandbiostratigraphyoftheBystricaandRaèasubunitsoftheMaguraNappehavebeen studied in the southern part of the Beskid Wyspowy Range and on the northern slopes of the Gorce Range (Polish part of the Western Flysch Carpathians). Six new lithostratigraphic units (Jasień Formation, Białe Formation, Jaworzynka Formation, Szczawina Sandstone Formation, Krzysztonów Member, and Ropianka Formation) of the UpperAlbian–Palaeocene age have been established, and five other units (Malinowa Shale Formation, Hałuszowa Formation, Łabowa Shale Formation, Beloveza Formation, Bystrica Formation) have been additionally described. The newly created formations as well as the Malinowa Shale Formation and the Hałuszowa Formation have been included to a new Mogielica Group of units (Upper Albian–Palaeocene). This group of units passes upwards into the Beskid Group (Eocene–Oligocene).The Mogielica Group, spanning over 40 myrs, represents the turbidite depositional system, separated by highstand variegated clays which can be correlated with minor sequences in terms of sequence stratigraphy. The following biostratigraphic zones have been recognised in the Cretaceous–Lower/Middle Eocene deposits: Plectorecurvoides alternans, Bulbobaculites problematicus, Uvigerinammina jankoi, U. jankoi-C. gigantea, Caudammina gigantea, Remesella varians, Rzehakina fisistomata, Glomospira div. sp., and Saccamminoides carpathicus. A few lithostratigraphic units consisting of calcareous sediments have been correlated with the standard calcareous nannoplankton zonation and the chronostratigraphy.
Płaszczowina magurska, największa jednostka tektoniczna zewnętrznych Karpat Zachodnich (Fig. 1), jest całkowicie odkorzeniona od swego podłoża. Utwory serii magurskiej starsze od turonu znane są jedynie z jednostki Grajcarka (sukcesja magurska pienińskiego pasa skałkowego), wiercenia Obidowa IG-1 oraz z kilku niewielkich odsłonięć przy południowym obrzeżeniu okna tektonicznego Mszany Dolnej (Fig. 2, por. Birkenmajer & Oszczypko, 1989). W jednostce Grajcarka, ponad głębokowodnymi utworami jury górnej i neokomu, występuje “czarny flisz” formacji wronińskiej (alb-cenoman) oraz zielone łupki radiolariowe cenomanu (formacja hulińska) (Birkenmajer, 1977, por. Oszczypko et al., 2004). Szaro-zielone łupki plamiste albu-cenomanu, znane z południowego obrzeżenia okna tektonicznego Mszany Dolnej, zdefiniowane zostały w pracy jako formacja łupków z Jasienia. Formacja ta, o miąższości niemniejszej od kilkunastu metrów, zazębia się w stropie z łupkami czerwonymi formacji z Malinowej. W Beskidzie Wyspowym i Gorcach ponad łupkami pstrymi formacji z Malinowej (turon-santon/kampan) oraz poniżej łupków pstrych formacji z Łabowej (eocen dolny i środkowy) występują zróżnicowane facjalnie osady fliszowe, zaliczane dotychczas do różnych nieformalnych jednostek litostratygraficznych, takich jak: warstwy z Kaniny, piaskowce ze Szczawiny (strefa bystrzyck i raczańska) oraz warstwy z Jaworzynki (strefa raczańka i strefa Siar). Najwyższą pozycję stratygraficzną zajmują utwory tradycyjnie nazywane “warstwami inoceramowymi” lub ropianieckimi. Na podstawie szczegółowych badań lito- i biostratygraficznych wyżej wymienionych utworów kredy górnej i paleocenu, zaproponowano cztery nowe formalne jednostki litostratygraficzne w randze formacji: formację z Białego (dotychczasowe warstwy z Kaniny), formację piaskowców ze Szczawiny (dotychczasowe piaskowce ze Szczawiny), formację z Jaworzynki (dotychczasowe warstwy z Jaworzynki) oraz formację ropianiecką (dotychczasowe warstwy ropianieckie). Ponadto badano pięć innych górnokredowo-eoceńskich formacji: łupków z Malinowej, z Hałuszowej, łupków z Łabowej, beloweskiej i bystrzyckiej, które dodatkowo opisano. Wszystkie nowo zdefiniowane formacje oraz formacje: łupków z Malinowej oraz z Hałuszowej, włączono do nowo wydzielonej grupy Mogielicy (górny alb-paleocen). Grupa ta przechodzi w stropie w grupę beskidzką (eocen-oligocen) opisaną przez Bir- kenmajera & Oszczypkę (1989). Grupa Mogielicy, obejmująca okres czasowy liczący ponad 40 mln lat, reprezentowana jest przez turbidytowy system depozycyjny, ograniczony w stropie i spągu przez osady łupków pstrych, związanych z okresem wysokiego względnego poziomu morza. Wśród zespołów mikrofauny otwornicowej albu - dolnego/ środkowego eocenu, znalezionych w badanych utworach płaszczowiny magurskiej, rozpoznano większość poziomów biostratygraficznych opracowanych dla polskich Karpat zewnętrznych przez Gerocha & Nowaka (1984) oraz przez Olszewską (1997). Do tego schematu włączono również poziomy charakterystyczne dla utworów płaszczowiny magurskiej. Poziom Plectorecurvoides alternans (poziom interwałowy IZ) Definicja: dolna granica - pojawienie się gatunku Plectorecurvoides alternans Noth (w badanym materiale dolna granica nie jest uchwycona, odpowiada początkowi profilu sukcesji magurskiej), górna granica - pojawienie się Bulbobaculites problematicus (Neagu);

Źródło:

Annales Societatis Geologorum Poloniae; 2005, 75, 1; 27-69
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 92.

Tytuł:

Eocene flora and trace fossils from the Hruby Regiel section in the Tatra Mountains (Poland): Taxonomic revision of the Wiktor Kuźniar fossil plant collection

Autorzy:

Worobiec, G.
Jach, R.
Machaniec, E.
Uchman, A.
Worobiec, E.

Powiązania:

https://bibliotekanauki.pl/articles/139288.pdf

Data publikacji:

2015

Wydawca:

Polska Akademia Nauk. Czytelnia Czasopism PAN

Tematy:

fossil leaves
fossil fruits
trace fossils
foraminifera
biostratigraphy
palaeoecology
palaeoclimate
Late Eocene
Western Carpathians
skamielina
liść
owoc
skamieniałości śladowe
otwornice
biostratygrafia
paleoekologia
Karpaty Zachodnie
eocen

Opis:

Latest Eocene plant macrofossils and trace fossils collected a century ago by Wiktor Kuźniar are revised and their stratigraphical and palaeoecological meaning is re-considered. They derive from marine limestones and marls cropping out on the northern slope of the Hruby Regiel mountain in the Western Tatra Mountains. Leaves belonging to the families Fagaceae and Lauraceae and fruits of the palm Nypa are recognized. The co-occurrence of the planktonic foraminifer taxa Chiloguembelina cf. gracillima and Globigerinatheca cf. index and fruits of Nypa suggests a latest Eocene age of the fossil flora. The plant assemblage is typical of paratropical or subtropical evergreen forests in a warm and humid subtropical climate, recent counterparts of which occur in southeast Asia. The presence of Nypa is characteristic of mangroves. The good state of preservation of the leaves suggests coastline proximity during sedimentation of the plant-bearing deposits.

Źródło:

Acta Geologica Polonica; 2015, 65, 2; 203-226
0001-5709

Pojawia się w:

Acta Geologica Polonica

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 93.

Tytuł:

A contribution to the moss and liverwort flora of the Reberce Nature Reserve at the Przemysl Foothills (Western Carpathians, Poland)

Autorzy:

Staniaszek-Kik, M.
Zubel, R.
Fudali, E.
Rusinska, A.
Fojcik, B.
Voncina, G.
Stebel, A.
Szczepanski, M.

Powiązania:

https://bibliotekanauki.pl/articles/790583.pdf

Data publikacji:

2017

Wydawca:

Uniwersytet Przyrodniczy w Poznaniu

Tematy:

moss
liverwort
flora
epixylic species
protected species
primeval forest
endangered species
bryophyte
Dentario glandulosae-Fagetum association
Reberce Nature Reserve
Przemysl Foothill
Western Carpathians Mountains
Polska

Opis:

The paper presents the results of studies on bryophyte flora of the Reberce forest reserve located in the Przemyśl foothills. Thirty-three species of liverworts, 70 species and two varieties of mosses were found. Terrestrial (66 species) and epixylic (58) bryophytes formed the largest ecological groups in the reserve. Twenty-four protected species were also recorded, eight endangered bryophytes and six taxa considered as primeval forest species. The most interesting finds are: Bazzania trilobata, Buxbaumia viridis, Calypogeia suecica, Cephalozia catenulata, Frullania dilatata, Metzgeria conjugata, Nowellia curvifolia, Orthotrichum lyellii, O. stramineum, Trichocolea tomentella and Ulota crispa.

Źródło:

Steciana; 2017, 21, 1
1689-653X

Pojawia się w:

Steciana

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 94.

Tytuł:

Analiza tempa depozycji materiału detrytycznego w basenach sedymentacyjnych zachodnich Karpat zewnętrznych jako wskaźnik aktywności tektonicznej ich obszarów źródłowych
Tectonic activity of sediment source areas for theWestern Outer Carpathian basins—constraints from analysis of sediment deposition rate

Autorzy:

Poprawa, P.
Malata, T.
Oszczypko, N.
Słomka, T.
Golonka, J.
Krobicki, M.

Powiązania:

https://bibliotekanauki.pl/articles/2074424.pdf

Data publikacji:

2006

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

basen sedymentacyjny
depozycja
aktywność tektoniczna
Karpaty Zachodnie
Western Outer Carpathians
Mesozoic
Cainozoic
sediment source area
deposition rate

Opis:

Analysis of deposition rate were performed for synthetic sections, representing the upper Jurassic to lower Miocene sedimentary fill of the Western Outer Carpathian (WOC) basins. Calculated deposition rates differs in a range of a few orders of magnitude. During Tithonian to Berriasian-early Valanginian tectonic activity of the source areas supplying the Silesian Basin was related to the mechanism of syn-rift extensional elevation and erosion of horsts. General decay of source area activity in Valanginian to Cenomanian time was caused by regional post-rift thermal sag of the WOC. The Barremian to Albian phase of compressional uplift of the source area located north of the WOC lead to increase of deposition rate in some zones of the WOC basin. In Turonian to Paleocene time thick-skinned collision and thrusting took place south and south-west (in the recent coordinates) of the Silesian Basin causing very rapid, diachronous uplift of this zone, referred to as Silesian Ridge, resulting with high deposition rate in the Silesian Basin. At that time supply of sediments to the Magura Basin from south was relatively low, and the Pieniny Klipen Belt was presumably zone of transfer of these sediments. In Eocene the zone of collisional shortening in the WOC system was relocated to the south, causing rapid uplift of the Southern Magura Ridge and intense supply of detritus to the Magura Basin. Thrusting in the Southern Magura Ridge and collisional compression resulted with flexural bending of its broad foreland, being the reason for decrease of activity of both the Silesian Ridge and the source area at the northern rim of the WOC. The Eocene evolution of the Silesian Ridge is interpreted as controlled by both episodic tectonic activity and eustatic sea level changes. Contrasting development of the Southern Magura Ridge and the northern rim of Central Carpathians during Eocene stands for a palaeographic distance between the two domains at that time. During Oligocene and early Miocene a significant increase of deposition rates is observed for the basin in which sediments of the Krosno beds were deposited. This was caused by tectonic uplift of the source at the northern rim of the WOC, as well as the Silesian Ridge and the partly formed Magura nappe. The Miocene molasse of the WOC foredeep basin is characterised by notably higher maximum deposition rates than ones calculated for the flysch deposits of the WOC.

Źródło:

Przegląd Geologiczny; 2006, 54, 10; 878-887
0033-2151

Pojawia się w:

Przegląd Geologiczny

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 95.

Tytuł:

Warunki rozwoju i rozmieszczenie torfowisk w Kotlinie Orawsko-Nowotarskiej
Development conditions and distribution of peat bogs in the Orava-Nowy Targ Basin

Autorzy:

Łajczak, A.

Powiązania:

https://bibliotekanauki.pl/articles/2074702.pdf

Data publikacji:

2009

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Kotlina Orawsko-Nowotarska
Karpaty Zachodnie
torfowiska niskie
torfowiska wysokie
wypływy wód gruntowych
Orava-Nowy Targ Basin
Western Carpathians
low peat bogs
raised peat bogs
shallow groundwater circulation

Opis:

The Orava-Nowy Targ Basin is the only intramontane basin in the Carpathian Mountains, where numerous low and raised peat bogs developed in the Holocene. The peat bogs were originally comprising about 40% of the basin area. to became confined to 12%, in result of several centuries of exploitation of peat. On the basis of investigations on geomorphological location of the preserved relics of peat bogs, and reconstructions of their original extent, an attempt was made to identify natural environment factors which had the biggest influence on development of peat-forming process within the Orava-Nowy Targ Basin. The most important of these factors were found to be landforms of fluvioglacial and fluvial accumulation and their composition, as well climatic conditions. However, it should be stated that distribution of raised peat bogs appears to be mainly controlled by the mode of circulation of shallow groundwaters and location of their stable outflows. This is an aspect of development of peat bogs that has not been studied up to now.

Źródło:

Przegląd Geologiczny; 2009, 57, 8; 694-694
0033-2151

Pojawia się w:

Przegląd Geologiczny

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 96.

Tytuł:

Pebbles of siliceous clastics and siliceous rocks in conglomerates of flysch sequences (Albian, Cenomanian) in vicinity of the Povażska Bystrica town, Klape Unit, Pieniny Klippen Belt, Western Carpathians
Otoczaki klastycznych utworów krzemionkowych i skał krzemionkowych w zlepieńcach sekwencji fliszowych (alb, cenoman) w okolicy Povażskiej Bystricy, jednostka klapska, pieniński pas skałkowy, Karpaty Zachodnie

Autorzy:

Zat'ko, F.
Sykora, M.

Powiązania:

https://bibliotekanauki.pl/articles/183553.pdf

Data publikacji:

2006

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

otoczaki klastycznych skał krzemionkowych
silicyty
petrografia
zlepieńce kredowe
Pieniński Pas Skałkowy
Karpaty Zachodnie
pebbles of siliceous clastic rocks
silicites
petrography
Cretaceous conglomerates
Pieniny Klippen Belt
Western Carpathians

Opis:

Pebbles of siliceous clastic rocks were not particularly petrographically studied so far in the Cretaceous exotic conglomerates of the Western Carpathians. They occur in polymictic conglomerates representing sediments of gravity flows. The pebbles of clastic rocks are known continuously in many places of the Pieniny Klippen Belt (PKB). Their average content in the conglomerates is up to 25%. Analysed were mainly pebbles of sandstones and conglomerates. According to degree of mineralogical maturity, diagenesis and sometimes low degree of metamorphism we infer their pre--Mesozoic age. No fossils were found in the examined rocks. Some of them were turmalinized. Except of clastic sediments, radiolarites, lydites (rarely with silicified plant tissue), and jaspers were identified. According to microscopic study, the siliceous sandstones and conglomerates mostly consist of quartz, feldspars, lithoclasts, heavy minerals and matrix (often chloritic). Their compositons were plotted in triangular diagrams Q-F-L (Quartz, Feldspars, Lithoclasts). The diagrams were compared with the diagrams of similar clastic rocks which are known from the sequences of Tatricum, Veporicum, Hronicum and Gemericum. The diagrams of clastic rocks of the Pieniny Klippen Belt conglomerates are apparently different from those of clastic rocks of the Central and Inner Western Carpathians
Otoczaki egzotykowych skał krzemionkowych Karpat Zachodnich nie były do tej pory obiektem badań petrograficznych. Występują one w kredowych zlepieńcach polimiktycznych spływów grawitacyjnych i znajdywane są w wielu miejscach pienińskiego pasa skałkowego (PKB). Udział tych egzotyków w zlepieńcach może dochodzić do 25%, przy czym niektóre z nich są sturmalinizowane. Analizie poddano głównie otoczaki piaskowców i zlepieńców. Przy braku jakichkolwiek skamieniałości, w nawiązaniu do stopnia mineralogicznej dojrzałości otoczaków, stopnia diagenezy, jak również słabego metamorfizmu autorzy sugerują ich przedmezozoiczny wiek. W oparciu o badania mikroskopowe stwierdzono, że piaskowce i zlepieńce krzemionkowe zawierają głównie kwarc, skalenie, minerały ciężkie i niezidentyfikowane litoklasty, tkwiące w matriksie, często o charakterze chlorytowym. Sporadycznie występują fragmenty radiolarytów, lidytów (rzadko ze skrzemionkowanymi fragmentami flory) i jaspisy. Skład badanych egzotyków przedstawiono na diagramach trójkątnych (Q, F, L). Diagramy te były z kolei porównywane z diagramami sporządzonymi dla podobnych utworów klastycznych znanych z sekwencji Tatricum, Weporicum, Hronicum i Gemericum, co doprowadziło do wniosku, że egzotyki tego typu z PKB są zupełnie różne od utworów klastycznych Karpat Centralnych i Zachodnich

Źródło:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2006, 32, 1; 65-77
0138-0974

Pojawia się w:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 97.

Tytuł:

Wtórna sukcesja roślinności w kierunku bagiennej olszyny górskiej Caltho laetae-Alnetum (Zarz. 1963) Stuchlik na dawnych łąkach Beskidu Niskiego
Secondary succession towards grey alder bog forest Caltho laetae-Alnetum (Zarz. 1963) Stuchlik on the abandoned meadows in the Beskid Niski Mts. (Western Carpathians)

Autorzy:

Koczur, A.

Powiązania:

https://bibliotekanauki.pl/articles/1008757.pdf

Data publikacji:

2012

Wydawca:

Polskie Towarzystwo Leśne

Tematy:

Beskid Niski
laki gorskie
laki podmokle
sukcesja roslin
sukcesja wtorna
gorska olszyna bagienna
zespol Caltho-Alnetum
abandoned meadows
secondary succession
grey alder bog forest
beskid niski mts.
western carpathians

Opis:

On the abandoned wet meadows in the Beskid Niski Mts. secondary succession to the community Caltho laetae−Alnetum proceeds. In the initial phases of succession significant similarity between patches of meadows communities and grey alder bog forest in floristic composition and structure of vegetation is observed. Particular stages of succession (non−forest and forest) are characterized by occurrence of big group (43.5%) of shared species.

Źródło:

Sylwan; 2012, 156, 10; 784-791
0039-7660

Pojawia się w:

Sylwan

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 98.

Tytuł:

Fossils from the Silesian-Subsilesian series of the Polish Western Carpathians : the implications for changes in sea-level and the marine environment during the Albian-Turonian

Autorzy:

Szydło, A.
Jugowiec-Nazarkiewicz, M.
Olszewska, M.

Powiązania:

https://bibliotekanauki.pl/articles/2059811.pdf

Data publikacji:

2015

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

fossils
calcareous nannoplankton
environments
sea-level
anoxic and biotic events
Albian-Turonian
Subsilesian-Silesian zone
Western Outer Carpathians
Polska

Opis:

Fossils and exotics from the Albian-Cenomanian deposits of the Western Polish Carpathians are discussed in relation with changes in depositional environments. Environmental conditions were controlled by geotectonic activity, sea-level changes and also anoxic and biotic events. During the Albian-the Early Cenomanian, and in the Turonian the fall in sea level led to increased supply of coarse-grained material rich in siliceous and sometimes calcareous bioclasts and exotics. This cyclic process has contributed to changes in the marine biota. In the Albian monogenic foraminiferal assemblages with the surficial epifauna corresponding to the organic influx and oxygen deficiency (OAE 1b) were evolved into more variable associations including deep infauna, which indicated more aerobic conditions. Under these conditions also preserved planktonic and calcareous benthic fossils, which indicated the supply of terrigenous material from shallow-water environments and land. During the Albian-Turonian transition intensive subsidence and volcanic activity associated with eustatic sea-level rise led to intensive production of phytoplankton. The sea-surface productivity and enhanced upwelling resulted in expanded short-term oxygen minima at the end of the Albian (OAE 1d) and the Cenomanian (OAE 2). In the latter interval benthic forms almost extinct while siliceous and calcareous plankton survived. In the Turonian changes in sea-level and sedimentary regime led to recolonization of the basin bottom.

Źródło:

Geological Quarterly; 2015, 59, 1; 215--228
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 99.

Tytuł:

Sztuczne sieci neuronowe dla uzupełnienia danych w geofizyce otworowej - wybrane przykłady
Artificial Neural Networks for completing data in well logging - selected examples

Autorzy:

Jarzyna, J.
Opyrchał, A.
Mozgowoj, D.

Powiązania:

https://bibliotekanauki.pl/articles/183854.pdf

Data publikacji:

2007

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

profilowania geofizyki otworowej
sztuczne sieci neuronowe
czas interwałowy
gęstość objętościowa
oporność pozorna
Karpaty Zachodnie
well logging
artificial neural networks
transit interval time
bulk density
apparent resistivity
Western Carpathians

Opis:

Wykorzystano sztuczne sieci neuronowe do odtwarzania profilowań geofizyki otworowej. Na podstawie dostępnych profilowań geofizyki wiertniczej odtworzono czas interwałowy rejestrowany przy profilowaniu akustycznym, gęstość objętościową będącą wynikiem profilowania gamma-gamma oraz oporność pozorną. Wybrano perceptrony i wsteczną propagację błędu jako metodę nauczania. Najbardziej skuteczne przy odtwarzaniu parametrów okazały się perceptrony z kilkoma neuronami na wejściu i przynajmniej kilkoma neuronami w warstwie ukrytej. Miarą poprawności wyników dostarczanych przez sieci były podstawowe statystyki obliczane dla odtworzonych parametrów w porównaniu z wynikami pomiarów lub estymacji. Najtrudniejsze do opracowania okazały się interwały, w których skały miały skomplikowaną litologię i zróżnicowaną przynależność stratygraficzną. Wyniki wykorzystano dla potrzeb interpretacji sejsmicznej, grawimetrycznej i magnetotellurycznej.
Artificial Neural Networks were used for reconstruction of well logs. Transit interval time recorded during acoustic log, bulk density as a result of gamma-gamma log and apparent resistivity were reconstructed on the basis of available logs. Perceptrons were chosen and the back propagation method was applied as the most effective training algorithm. Perceptrons with a few input neurons and at least a few neurons in a hidden layer turned out in reconstructing parameters. Basic statistics calculated for the reconstructed parameters compared to the measured or estimated ones acted as measures of correctness of solutions delivered by the networks. Intervals containing rocks of complex lithology and diversified stratigraphy turned out to be the most difficult to interpret. Results were applied in seismics, gravimetric and magnetotelluric interpretations.

Źródło:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2007, 33, 4/1; 81-102
0138-0974

Pojawia się w:

Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 100.

Tytuł:

A glimpse into ancient food storage: Sequestrichnia and associated nucleocave Chondrites from Eocene deep-sea deposits

Autorzy:

Šamánek, J.
Vallon, L.H.
Mikuláš, R.
Vachek, M.

Powiązania:

https://bibliotekanauki.pl/articles/31341414.pdf

Data publikacji:

2022

Wydawca:

Polska Akademia Nauk. Instytut Paleobiologii PAN

Tematy:

paleontology
Zoophycos brianteus
Chondrites intricatus
Helminthopsis tenuis
Tubulichnium mediterranensis
Scolicia strozzii
Dactyloidites
Megagrapton irregulare
Planolites
Eocene
deep-sea deposit
Zoophycos
trace fossil
fossil
flysch
Western Carpathians Mountains
Czech Republic

Źródło:

Acta Palaeontologica Polonica; 2022, 67, 3; 767-779
0567-7920

Pojawia się w:

Acta Palaeontologica Polonica

Dostawca treści:

Biblioteka Nauki

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