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Tytuł:
The youngest deposits infilling the Gdów “embayment” (Carpathian orogenic front, south Poland) are not older than late Sarmatian-Pannonian
Autorzy:
Wójcik, Antoni
Garecka, Małgorzata Katarzyna
Malata, Tomasz
Pilarz, Monika
Powiązania:
https://bibliotekanauki.pl/articles/2059596.pdf
Data publikacji:
2021
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Carpathian orogenic front
Carpathian Foredeep
Neogene basin
Miocene
Gdów “embayment”
Opis:
The Gdów “embayment” is the most pronounced deflection along the northern boundary of the Carpathians. It is filled by the sandy clay deposits which used to be named the Skawina Formation or Chodenice beds or, locally, conglomerates (of Sypka Góra). Their stratigraphic position according to studies of foraminifers had been determined as Badenian. New results obtained from micropalaeontological material sampled at three exposures near Wiatowice, Jawczyce (Giewont) and Gdów (Sypka Góra), and based on boreholes, indicate a much younger age of for the deposits infilling the Gdów “embayment”. These studies show that the surface deposits are not older than Late Sarmatian/Pannonian (Serravalian/Tortonian). They also suggest a much later time for the last stages of the thrusting of the Carpathian Mountains over the Carpathian Foredeep.
Źródło:
Geological Quarterly; 2021, 65, 2; 65: 22
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Recognition of geological structures at Starunia palaeontological site and vicinity (Carpathian region, Ukraine) based on gravity surveys
Autorzy:
Porzucek, S.
Madej, J.
Powiązania:
https://bibliotekanauki.pl/articles/191495.pdf
Data publikacji:
2009
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
Starunia
Carpathian region
Ukraine
Opis:
In the early 20th century, relics of Pleistocene mammals were found near the village of Starunia. Gravity surveys performed in the place of the discovery revealed a low-density bed in the Miocene Vorotyshcha salt-bearing beds. The lowered density resulted from high halite content and probably an increased number of ozokerite veins. The localization of zoological relics can be attributed to the existence of this bed. Surface gravity surveys enabled scientists to determine its course and horizontal range. Gravity surveys also confirmed the existence of the Rinne fault. In the western part of the study area gravity modelling showed an interface between Miocene Vorotyshcha salt-bearing beds and Sloboda Conglomerates, differing in average bulk density. Geologic data indicate that this interface may have the form of an overthust rather than of a fault.
Źródło:
Annales Societatis Geologorum Poloniae; 2009, 79, No 3; 357-363
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Konwencja o ochronie i zrównoważonym rozwoju Karpat
The Convention for protection and sustainable development of Carpathian Mountains
Autorzy:
Kozłowski, Stefan
Powiązania:
https://bibliotekanauki.pl/articles/1963576.pdf
Data publikacji:
2004-12-31
Wydawca:
Uniwersytet Kardynała Stefana Wyszyńskiego w Warszawie
Tematy:
Karpaty
konwencja
Convention for protection and sustainable development of Carpathian Mountains
Carpathian Mountains
Opis:
The article comprehends the description of coming into being The Convention for the protection and sustainable development of the Carpathian Mountains. It leads the analysis of the essence of this Convention and shows its importance for this part of Europe and for Poland. The article points also at the perspective and the possibility of putting into the execution of Convention resolutions.
Źródło:
Studia Ecologiae et Bioethicae; 2004, 2, 1; 383-388
1733-1218
Pojawia się w:
Studia Ecologiae et Bioethicae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Reconstruction of the Miocene depositional architecture of the Carpathian Foredeep basin based on geophysical data
Autorzy:
Stefaniuk, Michał
Florek, Marzena
Maćkowski, Tomasz
Hadro, Piotr
Cygal, Adam
Pieniądz, Krzysztof
Łapinkiewicz, Artur P.
Wachowicz-Pyzik, Anna
Powiązania:
https://bibliotekanauki.pl/articles/24202121.pdf
Data publikacji:
2023
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
Carpathian Foredeep
Miocene
geophysical data
Opis:
The Carpathian Foredeep in Poland is divided into two parts, eastern and western, with different tectonic frameworks and conditions of the Neogene sedimentary fill. The boundary is the so-called Krakow Ridge associated with the contact of two regional tectonic units: Upper Silesian and Malopolska blocks. The width of the Foredeep varies regionally and significantly differs in the western and eastern parts. It was developed within the epi-Variscan platform. Two zones can be distinguished in the Foredeep: the inner (older) zone and the outer zone. The subject of the presented work is the eastern part of the outer zone of Foredeep located in front of the head of the Carpathian thrust and filled mainly by autochthonous Miocene formations. The meridional width of this zone of the basin varies from about 10 km in the vicinity of Krakow to nearly 100 km in the central part. Its tectonic framework is defined from the south and south-west by marginal structures of the Carpathian overthrust and tectonic units of the folded Miocene. From the north-east and north-west, the border is marked by a system of faults in the foreground of Roztocze Upland and the Holy Cross Mountains. In the Sub-Cenozoic basement, a set of large faults of NW-SE length, with different times of formation and activity, is marked. These faults locally define horst structures and tectonic grabens. Some of the faults continue under the Carpathians, under which there is also a system of transversal faults in relation to the main axis of the orogeny. The influence of the tectonic structures of the basement is noticeable within the Miocene cover by faults disappearing towards the surface and continuous deformations of the adaptive type. The outer foreland basin is filled with marine molasse type deposits of the unfolded autochthonous Middle Miocene with a thickness of up to approx. 3.500 m. The complex of Miocene formations is formed, in the lower, south-western and central part, by strongly differentiated submarine fan deposits accompanied by basin plain formations and gravitational flow deposits, including turbidite deposits characteristic of flysch sedimentation. The outer part of the fans smoothly transitions into the zone of fine-clastic sedimentation of the basin plain. Above the complex of submarine fan sediments, there are thick complexes of sediments of deltaic origin, which are also intensively variable facies, creating a set of channel (coarse-grained) and extra-channel (finegrained) facies. The highest, relatively thin part of the sediments is formed by shallow coastal shelf formations. Submarine fans and river deltas developed mainly in the zone of the south-western and southern coasts of the Miocene reservoir, surrounded by river mouths providing an abundant supply of material from the rising and eroded Carpathians. In the north-eastern and locally even in the middle part of the basin, sediments may appear, for which the feeding area was located in the hinterland of the northern and north-eastern coast of the Miocene Sea. The limited scope of extraction of drill cores resulting from the exploratory and exploitation nature of drilling makes it necessary to use borehole and surface geophysical data to reconstruct the depositional architecture. Processing and interpretation of geophysical data for a complex of Miocene sediments with such characteristics are problematic and ambiguous. Numerous sources of sedimentary material supply in the form of river mouths and submarine channels cause a significant diversification of the depositional architecture of the Miocene basin, making it difficult to trace uniform stratigraphic and lithological and facies boundaries. Sedimentary conditions cause, on the one hand, a certain monotony of the sediments, dominated by clastic formations, enriched by evaporate sediments horizons, and on the other hand, great lateral and depth facies differentiation. Geophysical well-logging data allows to recognize the lithological and facies variability of sediments and to determine the sequence of changes along the borehole trajectory. Seismic reflection data was used to track lateral variability. For the seismic reflective method, the reflective boundaries, characterized by a significant, abrupt change in acoustic impedance, are of primary importance. Within the Miocene basin, numerous reflective boundaries with high lateral variability and non-obvious stratigraphic identification are observed. In a complex of siliciclastic deposits, seismic wave reflections are recorded from the boundaries separating fine-grained lithofacies and medium- and coarse-grained facies. Due to the dominance of deltaic sediments and submarine fans in the depositional architecture of the Miocene complex, the regional continuity of such boundaries is problematic, and their unambiguous stratigraphic identification is practically impossible. To sum up, intense lithological and facies variability of clastic deposits, both lateral and vertical, should be expected within the Miocene complex. The sediments of individual fragments of submarine fans and deltas overlap each other, and there may also be overlaps with the sediments of neighboring fans. Such characteristics of the complex translate into a variable seismic pattern with numerous reflective boundaries and intense lateral variability of the seismic signal characteristics
Źródło:
Geotourism / Geoturystyka; 2023, 1-2 (72-73); 68--69
1731-0830
Pojawia się w:
Geotourism / Geoturystyka
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Artesian origin of a cave developed in an isolated horst: a case of Smocza Jama (Kraków Upland, Poland)
Autorzy:
Gradziński, M.
Motyka, J.
Górny, A.
Powiązania:
https://bibliotekanauki.pl/articles/191456.pdf
Data publikacji:
2009
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
speleogenesis
palaeohydrology
Carpathian foreland basin
Opis:
The cave of Smocza Jama located in the centre of Kraków is developed in the Wawel Horst built of Upper Jurassic limestone and surrounded by grabens with Miocene clays. The cave is composed of two series: the old one has been known for ages and the new one was discovered when an artificial shaft was mined in 1974. The new series comprises small chambers separated by intervening thin walls while the old series consists of three connected together spatial chambers. The cave abounds in extensively developed solution cavities – cupolas and ceiling pockets. The internal fine-grained deposits, predominantly representing clay fraction are built of illite, mixed layer illite-smectite, kaolinite and iron oxides. They are probably the residuum after dissolution of Jurassic limestone. The cave originated in phreatic condition due to water input from below. The new series represents juvenile stage of cave evolution. The water rose through fissure-rifts located in chamber bottoms, circulated convectionally within particular chambers, finally led to bleaching of intervening walls, and hence to connection of the neighbouring chambers. The evolution of the old series is far more advanced. The rounded solution cavities imply that the cave was formed by water of elevated temperature. The lack of coarse-grained fluvial deposits, Pleistocene mammal remains and Palaeolithic artefacts prove that the cave was isolated since its inception till Holocene time. The cave originated due to artesian circulation, when the Wawel Horst was covered by imper- meable Miocene clays. A foreland basin with carbonate basement, filled with fine-grained molasse-type deposits seems to be particularly favourable for the development of artesian caves.
Źródło:
Annales Societatis Geologorum Poloniae; 2009, 79, No 2; 159-168
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zarys historii obrządków wschodnich na północnych obszarach Królestwa Węgier
Autorzy:
Rapacki, Franciszek
Powiązania:
https://bibliotekanauki.pl/articles/645354.pdf
Data publikacji:
2013
Wydawca:
Polska Akademia Nauk. Instytut Slawistyki PAN
Tematy:
Ruthenians
Carpathian
Hungary
monastery
rite
Opis:
 Eastern rite churches in the northern areas of the Kingdom of Hungary – historical outline The article provides an overview of the history of Eastern rites in the northern areas of the Kingdom of Hungary, focusing chiefly on the historical-graphic position of Karpatho-Rusyn The lands belonging today to Slovakia and Carpathian Ukraine from the Middle Ages, and the division of Christianity into two branches, were populated by a large group of believers who did not recognize the supremacy of the Roman Church. It was only in the seventeenth and eighteenth centuries that the power of the popes was recognized in exchange for the preservation of their traditional, religious rites. The text reconstructs the specific societal fate of the region. The article discusses the issues of the colonization of the territory, the history of the local church institutions, the fate of this area of Europe during the times of the Reformation, the establishment of the union between the Orthodox Church and Rome, and finally the era of the emergence of modern nationalisms. This study clarifies the discourse of today’s social and national activists. It reconstructs contemporary narratives and myths and proposes an overview of the creation of the cultural and political amalgam on the slopes of the Carpathian Mountains while asking questions concerning the origins of religious syncretism.
Źródło:
Adeptus; 2013, 2
2300-0783
Pojawia się w:
Adeptus
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Selected aspects of modern seismic imaging and near-surface velocity model building in the area of Carpathian fold and thrust belt
Autorzy:
Dalętka, Andrzej Michał
Powiązania:
https://bibliotekanauki.pl/articles/1841756.pdf
Data publikacji:
2021
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
seismic imaging
seismic refraction
seismic forward modelling
Carpathian fold belt
Carpathian thrust belt
Opis:
Despite the increasing technological level of the reflection seismic method, the imaging of fold and thrust belts remains a demanding task, and usually leaves some questions regarding the dips, the shape of the subthrust structures or the most correct approach to velocity model building. There is no straightforward method that can provide structural representation of the near-surface geological boundaries and their velocities. The interpretation of refracted waves frequently remains the only available technique that may be used for this purpose, although one must be aware of its limitations which appear in the complex geological settings. In the presented study, the analysis of velocity values obtained in the shallow part of Carpathian orogenic wedge by means of various geophysical methods was carried out. It revealed the lack of consistency between the results of 3D refraction tomography and both the sonic log and uphole velocities. For that reason, instead of the industry-standard utilization of tomography, a novel, geologically-consistent method of velocity model building is proposed. In the near-surface part, the uphole velocities are assigned to the formations, documented by the surface geologic map. Interpreted time-domain horizons, supplemented by main thrusts, are used to make the velocity field fully-compatible with the litho-stratigraphic units of the Carpathians. The author demonstrates a retrospective overview of seismic data imaging in the area of the Polish Carpathian orogenic wedge and discusses the most recent global innovations in seismic methodology which are the key to successful hydrocarbon exploration in fold and thrust regions.
Źródło:
Geology, Geophysics and Environment; 2021, 47, 2; 71-93
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Analiza chemostratygraficzna różnowiekowych osadów budujących górotwór karpacki
Chemostratygraphic analyses of sediments from different ages composing the Carpathian mountain range
Autorzy:
Kowalska, Sylwia
Powiązania:
https://bibliotekanauki.pl/articles/31348245.pdf
Data publikacji:
2023
Wydawca:
Instytut Nafty i Gazu - Państwowy Instytut Badawczy
Tematy:
chemostratygrafia
pXRF
Karpaty
chemostratigraphy
Carpathian
Opis:
Artykuł prezentuje próbę przeprowadzenia analizy chemostratygraficznej dla różnowiekowych skał budujących górotwór karpacki. W pierwszej kolejności zdecydowano się stworzyć syntetyczny profil geologiczny dla osadów występujących we wschodniej części polskich Karpat. Wykorzystane próbki, w większości piaskowce, pochodziły z głównych poziomów stratygraficznych w obrębie jednostek skolskiej i śląskiej, gdzie zidentyfikowano skały od dolnej kredy po paleocen. Ze względu na dostępność materiału badawczego do badań wytypowano próbki o udokumentowanej stratygrafii z dwóch otworów, D-1 i H-1, zwracając głównie uwagę na ich klasyfikację stratygraficzną. Następnie dla porównania wykonano profil chemostratygraficzny dla otworu Kuźmina-1. Stwierdzono obecność bardzo dużego zróżnicowania składu chemicznego pomiędzy głównymi poziomami stratygraficznymi wyróżnianymi na podstawie badań paleontologicznych w badanych otworach, co pozwoliło wyznaczać zdecydowane granice pomiędzy poszczególnymi poziomami stratygraficznymi. Możliwość stworzenia unikalnych modeli chemostratygraficznych dla czterech analizowanych poziomów stratygraficznych: kredy górnej – senonu (warstwy inoceramowe), kredy górnej / paleocenu (warstwy istebniańskie), eocenu (warstwy pstre) oraz oligocenu (warstwy krośnieńskie) potwierdziło również wykonanie diagramu klasyfikacyjnego Herrona. Największe zróżnicowanie cech chemostratygraficznych uzyskano w przypadku utworów kredowych. Wstępnie badania wykonano w laboratorium akredytowanym Actlabs, tak aby móc później przeprowadzić ewaluację wyników uzyskanych za pomocą przenośnych spektrometrów (pXRF Titan, o zakresie pomiarowym od Mg do U, oraz pXRF Tracer, który umożliwia również pomiar zawartości Na, oba aparaty firmy Bruker). Potwierdzono, że wyraźne zróżnicowanie zawartości poszczególnych pierwiastków widoczne jest zarówno dla pierwiastków głównych, jak i śladowych. Pierwiastki najbardziej diagnostyczne to Na, Mg, Fe, K, Ca, również Si, choć w tym przypadku zakres zmienności jest nieco mniejszy. W przypadku pierwiastków śladowych są to S, P, Mn, Ti, Sr, Zr, Ba, Rb i Zn, które można również analizować za pomocą przenośnych spektrometrów pXRF. Wykonane porównanie wyników składu chemicznego uzyskiwanych przenośnym spektrometrem pXRF oraz w laboratorium Actlabs wykazało, że możliwe jest wykorzystanie na większą skalę samych pomiarów spektrometrem pXRF. Dla większości pierwiastków diagnostycznych uzyskano wystarczająco precyzyjne wyniki przy wykorzystaniu przenośnych spektrometrów pXRF.
The article presents an attempt to conduct a chemostratigraphic analysis of the different-age rocks that form the Carpathian orogen. First, it was decided to create a synthetic geological profile for sediments occurring in the eastern part of the Polish Carpathians. The samples, mostly sandstones, were sourced from the primary stratigraphic layers in the Skole and Silesian Units, where rocks from the Lower Cretaceous to the Paleocene were identified. Due to the availability of research material, samples with well-documented stratigraphy were chosen from two wells, D-1 and H-1, with a particular focus on their stratigraphic classification. Subsequently, for comparison, a chemostratigraphic profile was generated for the Kuźmina-1 well. The analysis revealed significant disparities in chemical composition among the primary stratigraphic layers, which had been distinguished through paleontological studies in the examined boreholes. This made it possible to establish distinct boundaries between individual stratigraphic layers. The ability to create distinct chemostratigraphic models for the four examined stratigraphic horizons: Upper Cretaceous – Senonian (Inoceramian Beds), Upper Cretaceous/Paleocene (Istebnian Beds), Eocene (Variegated Shales), and Oligocene (Krosno Beds) was also confirmed through the creation of a Herrón classification diagram. The greatest variability of chemostratigraphic characteristics was observed in the Cretaceous formations. Initially, the tests were carried out in an accredited laboratory at ACTLABS, enabling the subsequent evaluation of results obtained using portable spectrometers (pXRF Titan, covering a measurement range from Mg to U, and pXRF Tracer, capable of also measuring Na content, both manufactured by Bruker). It was confirmed that clear variations in the content of individual elements were discernible for both major and trace elements. The most diagnostic elements include Na, Mg, Fe, K, Ca, and also Si, although the variability range is slightly narrower for the latter element. As for trace elements, these comprise S, P, Mn, Ti, Sr, Zr, Ba, Rb, and Zn, which can also be analyzed using portable pXRF spectrometers. A comparison between the chemical composition results obtained with the portable pXRF spectrometer and those from the ACTLABS laboratory revealed the feasibility of using pXRF measurements on a larger scale. For most diagnostic elements, sufficiently precise results were obtained using pXRF.
Źródło:
Nafta-Gaz; 2023, 79, 10; 623-639
0867-8871
Pojawia się w:
Nafta-Gaz
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Badenian tuffite levels within the Carpathian orogenic front (Gdów-Bochnia area, Southern Poland): radio-isotopic dating and stratigraphic position
Autorzy:
Bukowski, K.
de Leeuw, A.
Gonera, M.
Kuiper, K. F.
Krzywiec, P.
Peryt, D.
Powiązania:
https://bibliotekanauki.pl/articles/2059026.pdf
Data publikacji:
2010
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Miocene
Badenian
Carpathian Foredeep
tuffites
dating
Opis:
We present new results of investigation of Middle Miocene Badenian tuffite levels exposed in Southern Poland within the Gdów "embayment" area (tuffites from Wiatowice, upper part of the Skawina Beds, foraminiferal biozone IIg) and compare them with the well known and extensively described Bochnia Tuffite level at Chodenice near Bochnia (upper part of the Chodenice Beds, foraminiferal biozone IIIA). The 4039
Źródło:
Geological Quarterly; 2010, 54, 4; 449-464
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Reinterpretation of the results of the two-cycle reservoir test of the Mesozoic water-bearing deposits in the W-3 well in terms of assessing the changes in rock permeability in the zones tested with a drill stem tester
Autorzy:
Dubiel, S.
Rzyczniak, M.
Solecki, M. L.
Powiązania:
https://bibliotekanauki.pl/articles/299295.pdf
Data publikacji:
2018
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
Carpathian Foredeep
DST result
rock permeability
Opis:
The article presents the results of the reinterpretation of the results of the two-cycle DST of the Mesozoic strata in the W-3 well to assess the changes in permeability of reservoir rocks in the test zone. Two-dimensional diagrams of the first and second pressure restoration curves in the semi-logarithm coordinate system were taken into account. The determined linear regression equations of these sections give simultaneously the extrapolated value of the reservoir pressure and the directional coefficient. The “logarithmic approximation” method used in hydrogeology was used to determine the radius of the perimeter zone with altered permeability of the water-bearing rocks of the Mesozoic.
Źródło:
AGH Drilling, Oil, Gas; 2018, 35, 1; 57-68
2299-4157
2300-7052
Pojawia się w:
AGH Drilling, Oil, Gas
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Profesor Bronisława Kopczyńska-Jaworska a badania wsi
Professor Bronisława Kopczyńska-Jaworska and the Countryside Research
Autorzy:
Kuźma, Inga B.
Powiązania:
https://bibliotekanauki.pl/articles/966771.pdf
Data publikacji:
2017
Wydawca:
Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego
Tematy:
fieldwork
village
Carpathian Region research
letters
Opis:
This article concerns a fragment of research interests of the ethnographer from Lodz – professor Jaworska. In fact, Jaworska neither created the methodological theory of doing an ethnographical field research in a rural socio-cultural context nor the special theory connected with rural study, despite the fact that the most important area for her (in terms of science as well as her personal interests) were the Carpathian villages and the type of pastoral economy. The author of the text analyzes the letters of Jaworska written over 40 years, which reflect Jaworska’s attitude to her mountain field work carried out there as well as to the area itself.
Źródło:
Zeszyty Wiejskie; 2017, 23; 23-32
1506-6541
Pojawia się w:
Zeszyty Wiejskie
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Landslide processes in a flysch massif - case study of the Kawiory landslide, Beskid Niski Mts. (Carpathians, Poland)
Autorzy:
Zabuski, L.
Wójcik, A.
Gil, E.
Mrozek, T.
Raczkowski, W.
Powiązania:
https://bibliotekanauki.pl/articles/2059216.pdf
Data publikacji:
2009
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Carpathian flysch
landslide
monitoring
numerical simulation
Opis:
Geological setting and precipitation triggers seem to be obvious parameters controlling landslides, but their relation to individual sliding processes has not been clear. We take on interdisciplinary approach (combining Earth science methods with an engineer ing-geotechnical approach) to examine sliding processes in the Kawiory landslide in the Polish Carpathians. Field parameters were obtained from inclinometer monitoring, meteorological records, piezometer data and geomechanical tests. Numerical simulation of the landslide development was performed, both for the reconstruction of the internal deformation phenomena on the slope and for approximate prediction of its future behaviour. An empirical formula describing the relationship between the depth of groundwater level (GWL) and precipitation is presented. The case study showed that for the ob served quasi-continuous creep, the depth and in particular the intensity of GWL fluctuations might be crucial.
Źródło:
Geological Quarterly; 2009, 53, 3; 317-332
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Alabaster from the Carpathian Foredeep in the architecture of Cracow
Autorzy:
Rajchel, J. M.
Śliwa, T.
Wardzyński, M.
Powiązania:
https://bibliotekanauki.pl/articles/2060059.pdf
Data publikacji:
2014
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Carpathian Foredeep
Miocene
architecture
Cracow
Zhuravno
Opis:
Alabaster is a rock with low hardness, high coherence, fine-crystalline development and forms an optically “warm” surface when polished. It has been used as a sculpting, decorative and architectonic stone, often by civilizations of the Mediterranean Sea Basin. Alabaster in the architecture and sculpture of Kraków is mainly from the Middle Miocene (Badenian) and comes from deposits within the Ukrainian Carpathian Foredeep Basin, chiefly along its northern margin in the “Podolia rim”. It was quarried around the mid-part of the Dnister River and its tributaries, from Lviv (Lwów) to Khotyn (Chocim), and mostly at Zhuravno (Żurawno). The alabaster quarried here was called Ruthenian, Polish, or Lvov “marble”. Small quarries were also located at the front of the Carpathian overthrust, including the known deposit at Łopuszka Wielka. The Miocene alabaster has shades of white, yellow, green, brown, usually with differing spots or veins; often the rock is brecciated and partly semi-transparent. Alabaster has been quarried in the Polish Republic since the 16th century, peaking (also in finished stone products) between the world wars. The authors present examples of alabaster usage in ecclesiastical edifices of Kraków, for instance in the Wawel Cathedral, St. Mary’s Church, the churches of Dominican, Carmelite and Missionary clergy, and also in some secular buildings, e.g. the Jagiellonian Library.
Źródło:
Geological Quarterly; 2014, 58, 3; 597--616
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Late Pleistocene loess-paleosol and vegetation successions at Tarnawce (San River valley, Carpathians foothills, Poland)
Autorzy:
Komar, Maryna
Łanczont, Maria
Powiązania:
https://bibliotekanauki.pl/articles/2027418.pdf
Data publikacji:
2002
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Late Pleistocene
paleosol
loess
pollen
Carpathian Foothills
Opis:
The Tarnawce I profile, which occurs in the marginal eastern part of the Polish Westem Carpathians, contains loesses sq representing three last glacial cycles. In this paper we report the results of pollen analysis of the Eemian-Early Glacial pedocomplex and of the Lower plcni-Visrulian loesses with an interstadiał paleosol. The pollen spectra of22 samples were determined. The pollen diagram was divided into 7 local pollen assemblage zones (L PAZ). Interglacial climatic optimum was recorded with the Eemian type of vegetation in the T-4 zone. The coldest conditions occurred during the accumulation of loess, which separates the interglacial and interstadiał soils.
Źródło:
Studia Quaternaria; 2002; 27-35
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Lithostratigraphy and genesis of Quaternary strata between Lanckorona and Myoelenice in theWestern Outer Carpathians
Autorzy:
Grabowski, D.
Powiązania:
https://bibliotekanauki.pl/articles/2058804.pdf
Data publikacji:
2004
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Western Carpathian Foothills
Younger Pleistocene
lithostratigraphy
palaeosols
Opis:
The region between the Wieliczka Foothills and the Beskid Makowski Mts. has yielded new data on the accumulation of loess-like deposits during the Vistulian Glaciation. The grain-size distibution and the heavy mineral composition, particularly the significant presence of amphiboles, indicates on aeolian origin for these silty deposits. The silt was most probably derived from glaciofluvial deposits in the Carpathian forelands. Among the Quaternary deposits which accumulated during the Vistulian Glaciation and Holocene, three horizons of loess-like deposits (correlated with the lower, middle and upper younger loesses of the Lublin Upland), three horizons of solifluction deposits, and three horizons of deluvial deposits were distinguished. The accumulation of seven alluvial successions in the Raba and Harbutówka River valleys encompasses a large part of the Quaternary - from the South Polish Glaciations (terraces VII and VI) up to the Holocene (terraces II and I). The lithostratigraphy of the slope deposits (solifluctional and deluvial) and loess-like deposits has been estabilished mainly on the basis of 14C dates of the palaeosol horizons. One of these dates, combined with palynological analysis, confirmed the existence of a warmer period in the Denekamp Interstadial (31 200 +/- 1000 years BP in the Harbutowice-1 section). The dates obtained fromthe Jastrzębia-1 (20 760 +/- 300 years BP) and Polanka-1 (20 980 +/- 310 years BP and 14 510 +/- 150 years BP) sections point to periods favouring the development of soils in the younger and terminal parts of the Younger Pleniglacial. These results, consistent with the dates obtained by other investigators, point to the existence of a warmer period (between 24-20 ka BP) in southern Poland during the maximum development of the ice sheet (Main Stadial) during the last glaciation in northern Poland.
Źródło:
Geological Quarterly; 2004, 48, 4; 351--370
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 315

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