Results 131 to 140 of about 190,285 (154)
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Palaeogeography, Palaeoclimatology, Palaeoecology, 2019
A continuous sedimentary and stratigraphic record of Late Kimmeridgian – Early Berriasian age is presented from the pelagic succession from the eastern part of the Pieniny Klippen Belt (Velykyi Kamianets section, Ukraine). The studied section, 26-m-thick,
J. Grabowski +8 more
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A continuous sedimentary and stratigraphic record of Late Kimmeridgian – Early Berriasian age is presented from the pelagic succession from the eastern part of the Pieniny Klippen Belt (Velykyi Kamianets section, Ukraine). The studied section, 26-m-thick,
J. Grabowski +8 more
semanticscholar +1 more source
Geodynamic studies in the Pieniny Klippen Belt in 2004-202
2023The Pieniny Klippen Belt is located in the middle part of the zone between the Inner Carpathians and Outer Carpathians. Researches at the Pieniny Geodynamic Test Field dates back to the 1960s.Previous geodynamic studies in the area of the Pieniny Klippen Belt  have indicated neotectonic activity.
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New data on the age and stratigraphic relationships of the Czajakowa Radiolarite Formation in the Pieniny Klippen Belt (Carpathians) based on the radiolarian biostratigraphy in the stratotype section [PDF]
, 2018 The radiolarian biostratigraphy of the Middle–Upper Jurassic pelagic siliceous sediments (Czajakowa Radiolarite Formation) in the Niedzica succession of the Pieniny Klippen Belt (Carpathians) is interpreted in terms of their age in a stratotype section ...
M. Bąk +3 more
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Geology and Geochemistry of Combustible Minerals
New data obtained as a result of geological mapping conducted in recent years, together with the analysis of literary sources, made it possible to distinguish the Late Cretaceous-Paleogene active margin of the Alkapa microcontinental terrane. Fore-Alkapa
O. Hnylko
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New data obtained as a result of geological mapping conducted in recent years, together with the analysis of literary sources, made it possible to distinguish the Late Cretaceous-Paleogene active margin of the Alkapa microcontinental terrane. Fore-Alkapa
O. Hnylko
semanticscholar +1 more source
SCIENTIFIC PAPERS OF DONNTU Series: “The Mining and Geology”, 2023
Purpose of the paper is study of faults and folds and reconstruction of paleostress fields in rock complexes of the Pieniny Klippen Belt in Pieniny Mts. area (Southern Poland). Methods of field geological and structural research were involved, including the kinematic method with subsequent reconstruction of paleostress fields using the program Win ...
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Purpose of the paper is study of faults and folds and reconstruction of paleostress fields in rock complexes of the Pieniny Klippen Belt in Pieniny Mts. area (Southern Poland). Methods of field geological and structural research were involved, including the kinematic method with subsequent reconstruction of paleostress fields using the program Win ...
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Acta Geophysica, 2006
Middle-Upper Jurassic carbonates exposed in 7 separate fragments of three tectonic units were sampled in the Polish segment of the Pieniny Klippen Belt in 1981, before construction of the Niedzica-Czorsztyn dam. Demagnetization experiments performed about 20 years ago and analyzed lately with modern program package revealed the presence of Middle ...
Jadwiga Kruczyk +1 more
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Middle-Upper Jurassic carbonates exposed in 7 separate fragments of three tectonic units were sampled in the Polish segment of the Pieniny Klippen Belt in 1981, before construction of the Niedzica-Czorsztyn dam. Demagnetization experiments performed about 20 years ago and analyzed lately with modern program package revealed the presence of Middle ...
Jadwiga Kruczyk +1 more
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Sedimentary Geology, 2009
Abstract Four occurrences of Jurassic stromatactis mud-mounds were found in the Czorsztyn Unit of the Pieniny Klippen Belt (Western Carpathians) — in western Slovakia (Slavnicke Podhorie, Babina), and in the Transcarpathian Ukraine (Priborzhavskoe and Veliky Kamenets). Their stratigraphic range is from Bajocian to Callovian.
R. Aubrecht +5 more
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Abstract Four occurrences of Jurassic stromatactis mud-mounds were found in the Czorsztyn Unit of the Pieniny Klippen Belt (Western Carpathians) — in western Slovakia (Slavnicke Podhorie, Babina), and in the Transcarpathian Ukraine (Priborzhavskoe and Veliky Kamenets). Their stratigraphic range is from Bajocian to Callovian.
R. Aubrecht +5 more
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Albian and Cenomanian foraminifera from the Pieniny Klippen Belt (Carpathians, Poland)
1992A local stratigraphic zonation based on planktonic foraminifera has been established for the almost uninterrupted sequences of Albian to Cenomanian sediments of the Polish part of the Pieniny Klippen Belt. The assemblages resemble those of the Southern Alps and the Umbria-Marche Apennins.
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Cretaceous Research, 1988
Abstract Seven local biostratigraphic zones have been distinguished in the Albian and Cenomanian sediments of the Pieniny Klippen Belt: Hedbergella assemblage (Assemblage Zone, AZ), R. subticinensis-R. ticinensis (Concurrent Range Zone, CRZ), R. ticinensis- P. praebuxtorfi (CRZ), R. ticinensis- P.
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Abstract Seven local biostratigraphic zones have been distinguished in the Albian and Cenomanian sediments of the Pieniny Klippen Belt: Hedbergella assemblage (Assemblage Zone, AZ), R. subticinensis-R. ticinensis (Concurrent Range Zone, CRZ), R. ticinensis- P. praebuxtorfi (CRZ), R. ticinensis- P.
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