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Tytuł:
Sediment transport along the gullies in flysch badlands : an example from SW Slovenia
Autorzy:
Zorn, M.
Powiązania:
https://bibliotekanauki.pl/articles/295196.pdf
Data publikacji:
2011
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
badlands
gullies
erosion processes
flysch
Istria
Slovenia
Opis:
Sediment transport along erosion gullies in flysch badlands under Sub-Mediterranean climate is presented. Presented are weekly measurements, compiled measurements by months, as well as correlations of sediment transport with selected weather data. Sediment transport was measured up to 19 kg m-2 and was largely dependent on special weather conditions.
Źródło:
Landform Analysis; 2011, 17; 229-235
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The position and age of flysch deposits in the Crimean Mountains (Southern Ukraine)
Autorzy:
Oszczypko, N.
Ślączka, A.
Bubniak, I.
Olszewska, B.
Garecka, M.
Powiązania:
https://bibliotekanauki.pl/articles/2060566.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Ukraine
Crimean Mts.
stratigraphy
micropalaeontology
flysch
Opis:
The Crimean Mountains (CM) are regarded as part of the Alpine-Himalaya orogenic belt related to the collision of the Eurasian and African plates. Our research in the CM has allowed confirming the existence of at least two flysch formations of different ages: the Taurida Flysch Formation (Upper Triassic/Lower–? Middle Jurassic) and the Sudak Formation (uppermost Jurassic/Lower Cretaceous) in the western and eastern sectors of the CM, respectively. After the Middle Jurassic volcanism, the freshwater claystones with coal-bearing intercalations, as well as local alluvial fan conglomerates were deposited. Then, following the Oxfordian/Kimmeridgian marine transgression, three separated Tithonian/Berriasian carbonate platforms developed: Baydarska, Chatyr-Dag and Demerji/Karabi. At the turn of the Late Jurassic, the deep-water Sudak Basin (eastern sector of the CM) began to develop in the eastern periphery of the Demerji/Karabi carbonate platform. This basin, dominated by turbiditic deposition, was probably connected with the Great Caucasus sedimentary system. Finally, distal flysch sedimentation in the Sudak Basin was followed by debris-flow deposits, with huge blocks of Upper Jurassic limestones. These blocks were derived from destruction of the Karabi carbonate platform. During the Berriasian/Valanginian, the eastern sector of the CM began to subside. As a result, both carbonate platforms (western CM) and the debris flow fans of the Sudak Basin (eastern CM) were overlain by marly shales and/or distal turbidites. This type of deposition lasted until the Aptian/Albian. In the post-Albian period, the Alushta-Salgir tectonic zone was transformed into a SE-dipping thrust fault with at least 10 km amplitude of overthrusting.
Źródło:
Geological Quarterly; 2017, 61, 4; 697--722
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Advantages and limitations of interpretations of external morphology of detrital zircon: a case study of the Ropianka and Menilite formations (Skole Nappe, Polish Flysch Carpathians)
Autorzy:
Salata, D.
Powiązania:
https://bibliotekanauki.pl/articles/191222.pdf
Data publikacji:
2014
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
detrital zircon
morphology
flysch
Skole Nappe
Outer Carpathians
Opis:
The zircon populations from the Campanian–Maastrichtian part of the Ropianka (Upper Cretaceous– Palaeocene) and Menilite (Oligocene–lower Miocene) formations in the northern part of the Skole Nappe in Poland were examined to evaluate interpretations of the external morphology of detrital zircon in provenance research. The advantage of the zircon typology method, supplemented with elongation measurements, is that it may be applied successfully to comparisons of euhedral zircon populations from sedimentary deposits of different ages and unknown provenance. The zircon typology method, along with elongation measurements of zircons, contributes valuable data that supplement conventional heavy-mineral analyses. It also permits the recognition of potential source areas and rock types for further comparative research.
Źródło:
Annales Societatis Geologorum Poloniae; 2014, 84, 2; 153-165
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Source rocks for heavy minerals in lower part of Menilite Formation of Skole Nappe (Polish Flysch Carpathians), based on study of detrital garnet and tourmaline
Autorzy:
Salata, D.
Powiązania:
https://bibliotekanauki.pl/articles/191968.pdf
Data publikacji:
2013
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
detrital tourmaline
detrital garnet
provenance
flysch
Menilite Formation
Oligocene
Skole Nappe
Opis:
The study focused on the chemistry of detrital garnet and tourmaline from sediments of the Boryslav and Kliva Sandstone types in the Oligocene part of the Menilite Formation of the Skole Nappe (Western Outer Carpathians, Poland), with regard to provenance. Almandine and almandine-pyrope compositional varieties are the most common garnets, with minor almandine-pyrope-grossular garnet. Scarce garnet grains, with grossular and spessartine as the dominant end-members, are also present. The tourmaline belongs to the alkali tourmaline principal group and represents the schörl-dravite series. The detrital garnet and tourmaline display strong, compositional similarities to minerals, occurring in igneous and metamorphic rocks of the Bohemian Massif, as well as to detrital grains, deposited within the internal basins of the massif. This suggests that the primary rocks for the garnet and tourmaline may be crystalline complexes of the Bohemian Massif. However, other uplifted areas, similar to the complexes of the Bohemian Massif, cannot be ruled out. Such hypothetical areas could be located in the northern foreland of the Carpathian basins. Euhedral tourmaline and other minerals, occurring in the heavy- mineral assemblages studied, most probably were derived from eroded and presently not exposed, crystalline complexes, originally situated in the Skole Basin foreland or within the basin.
Źródło:
Annales Societatis Geologorum Poloniae; 2013, 83, 1; 1-17
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Szyszka drzewiastej rośliny widłakowej z dolnokarbońskiego fliszu Gór Bardzkich (Sudety)
Arborescent lycopsid cone from Lower Carboniferous flysch of the Bardo Mts (Sudetes)
Autorzy:
Muszer, J.
Haydukiewicz, J.
Powiązania:
https://bibliotekanauki.pl/articles/2074433.pdf
Data publikacji:
2006
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
stratygrafia
osad fliszowy
kłos zarodnikowy
Góry Bardzkie
stratigraphy
Carboniferous
Bardo Mts.
flysch
Lycopsida
Opis:
The Lower Carboniferous sediments of the Bardo Mts. is mainly composed of biostratigraphically undocumented flysch sequences. A cone impression was found in clayey-mudstone bed of the Srebrna Góra formation that represents one of these flysch sequences. The estimated Middle or even Upper Viséan relative age of this formation was determined based on the underlying paleontologically documented Nowa Wieś formation. The strobilus specimen is morphologically similar to cones assigned to genera Flemingites and Lepidostrobus, that were produced by arborescent lycopsids. The absence of in situ spores makes a precicse taxonomical determination of the cone impossible. The currently known stratigraphical ranges of the two genera are consistent with the previous opinions on the age of Srebrna Góra formation.
Źródło:
Przegląd Geologiczny; 2006, 54, 11; 963-966
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Transgraniczny geopark Karpaty fliszowe i ich wody mineralne
Flysch Carpathians and their mineral waters cross-border geopark
Autorzy:
Miśkiewicz, K.
Golonka, J.
Waśkowska, A.
Doktor, M.
Słomka, T.
Powiązania:
https://bibliotekanauki.pl/articles/2074884.pdf
Data publikacji:
2011
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
geopark
wody mineralne
Karpaty zewnętrzne
flisz
waloryzacja
spa
geoturystyka
mineral waters
flysch
valorization
geotourism
Opis:
The occurrence of mineral waters and related spas constitutes the leading theme of the projected geopark: Flysch Carpathians and their mineral waters. The geopark is located on the Beskid Sądecki and Beskid Niski area on the Polish side. It is situate in the area of the occurrence of three Carpathian units: Magura Nappe (the major part of the area), which includes Krynica, Bystrica, Racza and Siary tectonic-facies zones; Silesian Nappe and Grybów Unit. Besides mineral waters, the geodiversity of the area is defined by well exposed flysch rocks profiles including clastic type localities of the Magura Nappe described in the XIX century pioneers of geological investigations. The landslide morphology, attractive geomorphological forms like waterfalls, diversified river valleys, tors as well as places connected with history and tradition of exploration and exploitation of Carpathian hydrocarbons fields. The type localities of profiles of Grybów, Siary and Krynica Units as well as Łabowa Variegated Shales, Beloveza and Malcov formations. All these elements represent geotouristical attractions with high potential. They will be included in the network of preserved geosites within the projected geopark. The analysis of proposed geopark Flysch Carpathians and their mineral waters indicates high degree of diversification of natural values, especially geodiversity as well as richness of historical-cultural heritage. The preservation and protection methods are also diversified. This region represents unique geoenvironmental and historical values on the European scale, therefore providing good chances for establishment of geopark. The proposition of geopark with mineral waters and related spas in the Flysch Carpathians is first such project in the world. The documentation of geosites was already gathered during this stage of work, it requires only actualization, minor additions and construction of unified database. The evaluation of the actual touristic infrastructure provided also generally positive results, only the eastern part of geopark requires additional investments and promotion.
Źródło:
Przegląd Geologiczny; 2011, 59, 9; 611-621
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Garnet provenance in mixed first-cycle and poly-cycle heavy-mineral assemblages of the Ropianka and Menilite formations (Skole Nappe, Polish Flysch Carpathians): constraints from chemical composition and grain morphology
Autorzy:
Salata, D.
Powiązania:
https://bibliotekanauki.pl/articles/973614.pdf
Data publikacji:
2013
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
detrital garnet
mixed provenance
protolith location
flysch
Skole Nappe
Carpathians
Opis:
Garnet in heavy-mineral assemblages, occurring in sandstones of the Campanian–Maastrichtian part of the Ropianka (Late Cretaceous–Palaeocene) and Menilite (Oligocene) formations of the Skole Nappe, is present as first-cycle and poly-cycle grains, derived from a proximal source, remote areas and/or from sedimentary rocks of the Skole Basin foreland. The garnets in the formations are compositionally similar, suggesting an origin from the same source rocks. Relatively large amounts of garnet, represented by euhedral or slightly rounded, weakly etched or unetched almandine and spessartine-almandine garnet, and minor pyrope-enriched almandine, were derived directly from a source close to the Skole Basin. These garnets are from sediments, metamorphosed at low- to medium-grade conditions (such as mica-schists, gneisses) and perhaps also granitic bodies. Rounded and variously etched garnets, especially high pyrope-almandine and pyrope-almandine-grossular varieties, but also partly almandine-dominated varieties, are suggested to have been derived from distant sources, such as sedimentary rocks of the Upper Silesian and Małopolska blocks. Rocks, forming uplifted parts of the crystalline basement of Brunovistulicum and/or crystalline domains of the Bohemian Massif, could have been protoliths for part of the almandine-dominated garnet population, whereas pyrope-grossular-almandine garnets may originate from the granulitic, eclogitic or metabasic rocks of the Bohemian Massif. The study shows that analyses of garnet composition, combined with observations on grain textural features and data on the lithology of clasts and pebbles, can permit the determination of sources for different garnet varieties in mixed-provenance populations.
Źródło:
Annales Societatis Geologorum Poloniae; 2013, 83, 3; 161-177
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Conventional and high-resolution heavy mineral analyses applied to flysch deposits : comparative provenance studies of the Ropianka (Upper Cretaceous–Paleocene) and Menilite (Oligocene) formations (Skole Nappe, Polish Carpathians)
Autorzy:
Salata, D.
Uchman, A.
Powiązania:
https://bibliotekanauki.pl/articles/2060326.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
heavy minerals
high-resolution
correlation
sedimentary provenance
flysch
Outer Carpathians
Skole Nappe
Opis:
Conventional and high-resolution analyses of heavy minerals from the gravity flow-deposited sandstones of the Campanian–Maastrichtian interval of the Ropianka (Upper Cretaceous–Paleocene) and Menilite (Oligocene) formations of the Polish Carpathians display similar compositions in terms of mineral species. Zircon, tourmaline, rutile, garnet, staurolite and kyanite belong to the main constituents in both formations. Apatite is common in the Ropianka Fm., while the Menilite Fm. almost lacks this mineral. Furthermore, individual hornblende grains were found in the Ropianka Fm., while andalusite is present only in the Menilite Fm. The Ropianka Fm. is relatively richer in zircon, tourmaline, garnet and apatite, while the Menilite Fm. contains more staurolite and kyanite. Zircon and tourmaline colour and morphological varieties are similar in both formations. The similarities of the heavy mineral assemblages studied suggest origin of these minerals from lithologically similar rocks. Negative correlations between the zircon + tourmaline + rutile (ZTR) values and the content of garnet and staurolite in the Ropianka Fm. may indicate, to a large extent, first-cycle delivery of garnet and staurolite to the formation. Negative, but low, correlation valid only for ZTR and garnet and positive correlations for ZTR and staurolite and kyanite in the Menilite Fm. suggest delivery of these minerals from sedimentary rocks or/and palimpsest sediments. The data obtained on mineral relationships and their morphology suggest mixed first-cycle and recycled provenance of the heavy minerals studied. Additionally, the first-cycle material input seems to be larger during the Ropianka Fm. sedimentation, while during the deposition of Menilite Fm. the contribution of material delivered from erosion of recycled sediments appears more prominent. The heavy mineral evidence suggests a change at the northern margin of the Skole Basin from an immature passive margin with a high relief during sedimentation of the Campanian–Maastrichtian part of the Ropianka Fm. to a mature passive margin with a low relief during sedimentation of the Menilite Fm.
Źródło:
Geological Quarterly; 2013, 57, 4; 649--664
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wpływ opadu i infiltracji na zasilanie paleogeńskich poziomów wodonośnych w skałach fliszowych Beskidu Sądeckiego
Influence of precipitation and infiltration on recharge the Paleogene aquifers of the Beskid Sądecki flysch
Autorzy:
Buczyński, S.
Wcisło, M.
Powiązania:
https://bibliotekanauki.pl/articles/2062173.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
wahania zwierciadła wód podziemnych
opad
zasilanie
flisz
Karpaty
groundwater dynamics
precipitation
recharge
flysch
Carpathians
Opis:
W artykule przedstawiono wyniki badań wpływu opadów i infiltracji na zasilanie paleogeńskich poziomów wodonośnych w skałach fliszowych. Badania wskazują, że wielkość zasobów eksploatacyjnych w rejonie Tylicza wiąże się ściśle z reżimem zasilania, dlatego też w pracy określono terminy występowania stanów charakterystycznych zwierciadła wód podziemnych oraz amplitud wzniosu i spadku zwierciadła na tle wielkości opadów i infiltracji.
The paper describes research on the effect of precipitation and infiltration on the groundwater recharge of the Palaeogene aquifer. Since the safe yield in the Tylicz region is closely linked to the recharge regime, the dates of occurrence of specific groundwater levels and amplitudes of water table increase and decrease have been characterised. These data have been discussed on the background of precipitation and infiltration rates.
Źródło:
Biuletyn Państwowego Instytutu Geologicznego; 2013, 456 Hydrogeologia z. 14/1; 57--62
0867-6143
Pojawia się w:
Biuletyn Państwowego Instytutu Geologicznego
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ocena wodonośności utworów fliszowych w rejonie Muszyny na podstawie badań źródeł
Assessment of water-bearing capacity of flysch deposits in the Muszyna region based on spring investigation
Autorzy:
Józefko, I.
Oszczypko, N.
Kukuła, M.
Powiązania:
https://bibliotekanauki.pl/articles/2062248.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
wodonośność
źródła
wody podziemne
flisz
Muszyna
Karpaty
water-bearing capacity
springs
groundwater
flysch
Carpathians
Opis:
W pracy zaprezentowano wyniki badań hydrogeologicznych prowadzonych w rejonie Muszyny. Na podstawie analizy wyników badań naturalnych wypływów wód podziemnych, po uwzględnieniu budowy geologicznej i wyników badań hydrologicznych, oceniono wodonośność utworów fliszowych, co umożliwiło dyskusję na temat zmienności wodonośności na obszarze współwystępowania wód zwykłych i mineralnych.
This paper present the results of hydrogeological studies conducted in the Muszyna region. Based on the results of the analysis of natural groundwater discharges, and taking into account the geological structure and the results of hydrological studies, the water-bearing capacity of flysch rocks has been rated. This allowed discussing the water-bearing capacity in the area of drinking and mineral water co-occurrence.
Źródło:
Biuletyn Państwowego Instytutu Geologicznego; 2013, 456 Hydrogeologia z. 14/1; 233--241
0867-6143
Pojawia się w:
Biuletyn Państwowego Instytutu Geologicznego
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geotectonic significance of Carboniferous deposits NW of the Holy Cross Mts. (central Poland)
Autorzy:
Jaworowski, K.
Powiązania:
https://bibliotekanauki.pl/articles/2059900.pdf
Data publikacji:
2002
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Central Poland
Carboniferous
debrites
turbidites
flysch
pseudoflysch
Opis:
Carboniferous sandstones and shales encountered in deep boreholes drilled in central Poland, NW of the Holy Cross Mts., represent a pseudoflysch i.e. they show facies features of flysch and, simultaneously, are of cratonic provenance. Clastic sediments were derived from a peripheral bulge formed within the East European Craton as a result of stresses exerted by the accretion/thrust wedge advancing up the marginal part of the craton. In central Poland, NW of the Holy Cross Mts., a Variscan foredeep existed. The foredeep was the depositional site of interfingering exo- and pseudoflysch which, from a geodynamic point of view, are equivalent to an outer molasse. Huge masses of Carboniferous deposits (generally corresponding to flysch) from southwestern and central Poland successively represent, moving from SW to NE, Variscan ortho-, exo- and pseudoflysch.
Źródło:
Geological Quarterly; 2002, 46, 3; 267-280
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geopark „Beskid Śląsko-Morawsko-Żywiecki”- najstarsze utwory Karpat fliszowych
"Silesian-Moravian-Żywiec Beskid" Geopark – the oldest deposits of the Flysch Carpathians
Autorzy:
Golonka, J.
Krobicki, M.
Miśkiewicz, K.
Slomka, T.
Waśkowska, A.
Doktor, M.
Powiązania:
https://bibliotekanauki.pl/articles/2075059.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
geopark
geoconservation
Outer Carpathians
flysch
valorization
Silesian Nappe
Magura Nappe
geoochrona
Karpaty zewnętrzne
flisz
waloryzacja
płaszczowina śląska
płaszczowina magurska
Opis:
The oldest flysch deposits are the leading theme of the planned "Silesian-Moravian-Żywiec Beskid" Geopark. The geopark is located in the area of Beskid Śląski Mts. and Beskid Żywiecki Mts. in the territory ofPoland. This is a region of the occurrence of a number of tectonic units of the Outer Carpathians, including Pieniny Klippen Belt, Magura Nappe (with Krynica, Bystrica, Raca and Siary tec- tonic-facies zones), Fore-Magura Unit, Silesian Nappe and Subsilesian Nappe. Geodiversity of this area is defined by well-exposed sections ofrocks. They were the sites ofclassical geological work in the 19th century. Within the geopark boundaries, there are the type localities of the following tectonic units: Silesian Nappe, Fore-Magura, Bystrica and Raca units, as well as Jaworzynka, Bystrica, Vyhylovka, Vendryne and Cieszyn Limestone formations, Malinowska Skala Conglomerate, Mutne Sandstone, and Cisownica Shale members. Landslides, attractive geomorphologic landforms (e.g., highest peaks of the Beskidy Mts., providing magnificent views), waterfalls, diversified river valleys, tors, caves as well as places associated with the history and tradition of this region represent geotouristic attractions with a high potential. They will be included in the network ofgeosites protected within the planned geopark. Analysis ofthe geopark area indicates a high degree of variability of natural values, especially its geodiversity and richness of the historical-cultural heritage. The preservation and protection methods are also diversified. This region represents unique geoenvironmental and historical values on the European scale, therefore offering good chances for establishment of geopark. The documentation of geosites has already been gathered at this stage of work. The information requires only updating, minor additions and construction ofa unified database. The evaluation ofthe current touristic infrastructure have also brought very positive results; the area isfrequented by millions oftouristsfrom Poland, Czech Republic, Slovakia and other countries.
Źródło:
Przegląd Geologiczny; 2013, 61, 5; 277--285
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Tektonika polskich Karpat fliszowych pomiędzy Bielskiem-Białą a Nowym Targiem
Tectonics of the Polish Flysch Carpathians between Bielsko-Biała and Nowy Targ
Autorzy:
Golonka, J.
Powiązania:
https://bibliotekanauki.pl/articles/183840.pdf
Data publikacji:
2007
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
Karpaty zewnętrzne
flisz
tektonika
płaszczowina magurska
grupa płaszczowin przedmagurskich
płaszczowina śląska
płaszczowina podśląska
płaszczowina skolska
Outer Carpathians
flysch
tectonics
Magura Nappe
Fore-Magura Nappes
Silesian Nappe
Skole Nappe
Fore-Silesian Nappe
Opis:
Przedmiotem pracy są Karpaty zewnętrzne pomiędzy Bielskiem-Białą a Nowym Targiem. Zbudowane są one z silnie, płaszczowinowo sfałdowanych osadów fliszowych wieku jury górnej - neogenu. Wśród płaszczowin Karpat zewnętrznych wyróżnia się (idąc od południa): jednostkę (płaszczowinę) magurską, grupę płaszczowin przedmagurskich, płaszczowiny śląską, podśląską i skolską (grupa średnia). Jednostka magurska od południa, wzdłuż linii Stare Bystre - Szaflary, graniczy z pienińskim pasem skałkowym. Jest nasunięta na jednostki grupy średniej - wielkość nasunięcia wynosi co najmniej 20 km. Strefa przedmagurska ciągnie się wąskim pasem z rejonu Milówki w kierunku na południowe zbocze Beskidu Małego, gdzie zanika. Płaszczowina śląska podzielona jest wzdłuż uskoku Skawy na dwa odcinki. Zachodni charakteryzuje się potężnym rozwojem kredowych piaskowców godulskich, we wschodnim odsłaniają się na znaczniejszym obszarze warstwy krośnieńskie. Płaszczowina podśląska występuje w postaci porozrywanych strzępów i płatów pojawiających się u brzegu płaszczowiny śląskiej, jak również w oknach tektonicznych w obrębie jednostki śląskiej. Jednostka skolska występuje na północ od Wadowic i Andrychowa, gdzie tworzy element łuskowo nasunięty na miocen zapadliska przedkarpackiego.
The Polish Outer Carpathians between Bielsko-Biała and Nowy Targ are built up from the thrust, imbricated Upper Jurassic - Neogene flysch deposits. The following Outer Carpathian nappes have been distinguished: Magura Nappe, Fore-Magura group of nappes, Silesian, Subsilesian and Skole Nappes. The Magura Nappe borders along Stare Bystre-Szaflary line with the Pieniny Klippen Belt. It is thrust over the Fore-Magura and Silesian nappes at least 20 km. The Skawa line system of faults displaces the Magura Nappe margin 2 km northward. The Fore-Magura narrow zone runs from Milówka to the southern slope of Beskid Mały, where disappears from the surface. The Silesian Nappe is devided into two segments along the Skawa fault. The western one is characterized by the development of Cretaceous Godula Sandstones, eastern by the occurrence of Krosno Beds. The Sub-Silesian Nappe occurs as broken pieces along the northern margin of the Silesian Nappe, as well as in the tectonic windows within the Silesian Nappe. The Skole Unit is thrust over the Miocene deposits of Carpathian Foredeep in the area north of Wadowice and Andrychów.
Źródło:
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2007, 33, 4/1; 29-38
0138-0974
Pojawia się w:
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Development of fault pattern in the Silesian Nappe: Eastern Outer Carpathians, Poland
Autorzy:
Rubinkiewicz, J.
Powiązania:
https://bibliotekanauki.pl/articles/2059434.pdf
Data publikacji:
2000
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Polish Eastern Outer Carpathians
flysch
structural geology
fault slip analysis
Opis:
The development of fault pattern in the Silesian Nappe (Central Carpathian Depression) in the eastern part of Polish Outer Carpathians is outlined, from field observations and interpretation of air photos and radar images. Fault slip analysis and palaeostress reconstruction was applied to determine different systems of strike-slip, reverse and normal faults and the relative age of each system was determined. The results show a consistent evolution of fault systems which occurred as several episodes. Some of these episodes are local but others represent a regional pattern of faulting across the whole Polish Eastern Outer Carpathians. The beginning of fault evolution took place in Late Oligocene to Late Miocene times. The oldest phase is represented by reverse and thrust faults of system R1 with SW-NE compression; a younger phase involves origination of strike-slip faults belonging to system S1 (with the same direction of compression). Reverse (system R2) and strike-slip (system S2) faults were formed locally during a N-S compressional event. Dextral strike-slip faults of system S3 with simultanous opening of a dextral set of fault system S1 originated subsequently. The youngest events are represented by normal faults N1, N2, and N3 systems during NW-SE, and SW-NE to N-S extension.
Źródło:
Geological Quarterly; 2000, 44, 4; 391-403
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Palynostratigraphy of the Culm deposits of the Moravian-Silesian zone (Poland) at Toszek Castle Hill
Autorzy:
Trzepierczyńska, A.
Powiązania:
https://bibliotekanauki.pl/articles/2058834.pdf
Data publikacji:
2003
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Moravian–Silesian zone
Culm
flysch
palynostratigraphy
miospores
Serpukhovian
Opis:
The Early Carboniferous age of the flysch succession in the Moravian-Silesian zone has been based principally on lithological correlations with the stratotype goniatite-bearing section. Its uppermost part-the Kyjovice Formation in the region of Toszek (Poland)-has been studied palynologically for the first time. Miospore assemblages of the upper part of the Western European nitidus-carnosus (NC) miospore Zone of the early Serpukhovian have been distinguished. This agrees well with a general stratigraphic range of the Kyjovice Formation within the Go-E1a goniatite zones.
Źródło:
Geological Quarterly; 2003, 47, 4; 373-380
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 33

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