Zobrazeno 1 - 10 of 32 pro vyhledávání: '"Nestor Oszczypko"'
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The Early Miocene residual flysch basin at the front of the Central Western Carpathians and its palaeogeographic implications (Magura Nappe, Poland)
Autor: Anna Piecuch, Ján Soták, Józef Boratyn, Marta Oszczypko-Clowes, Nestor Oszczypko
Publikováno v: Geological Quarterly.
In the Polish sector of the Magura Nappe, along the front of the Pieniny Klippen Belt, strongly tectonized calcareous flysch up to 1000 m thick is exposed. Previously these deposits, composed of thin- to thick-bedded flysch, with a packet of Łącko-
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e422617ab24e413b7fcae534ebdefc13
https://doi.org/10.7306/gq.1425
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4
The position and age of flysch deposits in the Crimean Mountains (Southern Ukraine)
Autor: Nestor Oszczypko, Małgorzata Garecka, Barbara Olszewska, Andrzej Ślączka, Ihor Bubniak
Publikováno v: Geological Quarterly.
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 differe
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d7c5e7a29b537ac3e517cbcd707a43f0
https://doi.org/10.7306/gq.1359
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5
Neogene palaeogeography and basin evolution of the Western Carpathians, Northern Pannonian domain and adjoining areas
Autor: Michal Kováč, Emő Márton, Nestor Oszczypko, Rastislav Vojtko, Jozef Hók, Silvia Králiková, Dušan Plašienka, Tomáš Klučiar, Natália Hudáčková, Marta Oszczypko-Clowes
The data on the Neogene geodynamics, palaeogeography, and basin evolution of the Western Carpathians, Northern Pannonian domain and adjoining areas (ALCAPA Mega-unit) are summarized, re-evaluated, supplemented, and newly interpreted. The proposed con
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::634164f951d8218b3c5a0f299e2ac0e4
https://ruj.uj.edu.pl/xmlui/handle/item/45052
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6
Occurrence of Upper Jurassic–Lower Cretaceous black organic-rich pelitic sediments as targets for unconventional hydrocarbon exploration in the Outer Carpathians and adjacent part of the Alps
Autor: Marek Cieszkowski, Jan Golonka, Tadeusz Słomka, Andrzej Ślączka, Irena Matyasik, Nestor Oszczypko
Publikováno v: AAPG Bulletin. 98:1967-1994
Our work on the dark pelitic sediments of the Polish Carpathians and eastern Alps shows that these Jurassic through Lower Cretaceous sediments owe their organic content to a combination of global processes, such as climatic changes and changes to the
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e62b0568081c716d0fc23c27e2263fef
https://doi.org/10.1306/02211413049
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7
Exceptionally favourable life conditions for macrobenthos during the Late Cenomanian OAE-2 event: Ichnological record from the Bonarelli Level in the Grajcarek Unit, Polish Carpathians
Autor: Alfred Uchman, Nestor Oszczypko, Francisco J. Rodríguez-Tovar
Publikováno v: Cretaceous Research. 46:1-10
Pelagic and hemipelagic sediments of the Bonarelli Level (uppermost Cenomanian) in the Sztolnia section (Grajcarek Unit, Polish Carpathians) contain trace fossils of the Zoophycos ichnofacies, including (in descending order of abundance): Chondrites
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7afee635b94b8d13ab2f09b287e1791d
https://doi.org/10.1016/j.cretres.2013.08.007
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8
Structure and Miocene evolution of the Gdów tectonic 'embayment' (Polish Carpathian Foredeep) – a new model based on reinterpreted seismic data
Autor: Piotr Krzywiec, Nestor Oszczypko, Krzysztof Bukowski, Aleksander Garlicki
Publikováno v: Geological Quarterly. 56:907-920
Analysis of previously available stratigraphic data coupled with the re-interpretation of seismic profiles calibrated by boreholes has allowed the construction of a new tectonic model of evolution of the Gdow “embayment” – a tectonic re-entrant
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::965812c118703fee354a6fc6887e61f1
https://doi.org/10.7306/gq.1067
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9
Foreland provenance of thick conglomerates in the early stage of the Carpathian Foredeep development: the case of the Sloboda Conglomerate (Lower Miocene), western Ukraine
Autor: Ihor Bubniak, Alfred Uchman, Nestor Oszczypko
Publikováno v: Geological Quarterly. 56:789-802
The upper part of the Lower Miocene Sloboda Conglomerate, a 250-1400 m thick unit, was deposited mainly on an alluvial fan and fan delta during the early stages of Carpathian Foredeep development. During of the Old Styrian overthrust movements of the
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c779e339e7d2d9586896d7d47f467af3
https://doi.org/10.7306/gq.1055
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10
The Stebnyk Formation (Miocene) in the Boryslav-Pokuttya and Sambir nappes of the Ukrainian Carpathians : a record of environmental change in the Carpathian Foredeep
Autor: Nestor Oszczypko, Ihor Bubniak, Alfred Uchman
The late Early–Middle Miocene Stebnyk Formation is a ~600–2000 m thick unit of the Boryslav-Pokuttya and Sambir nappes, which contains a molasse succession of the Carpathian Foredeep incorporated within the marginal part of the Outer Eastern Carp
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9522b8c11d2287fc5c8d77399f85621a
http://ruj.uj.edu.pl/xmlui/handle/item/29065
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