Results 131 to 140 of about 1,578 (175)
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Mid Cretaceous Radiolaria from the Pieniny Klippen Belt, Carpathians, Poland
Cretaceous Research, 1995Abstract Aptian? to Early Turonian radiolarian faunas have been recovered from three sections in the Branisko succession of the Pieniny Klippen Belt, Carpathians. The species determined belong to the orders Spumellaria (14 species) and Nassellaria (34 species).
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Historical Biology, 2021
The tens of metres thick shell accumulations within the Cenomanian-Turonian strata of Western Carpathians enabled a complex study of ecological and geochemical proxies in relation to behavioural patterns of oyster Rhynchostreon suborbiculatum ...
Jakub Rantuch
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The tens of metres thick shell accumulations within the Cenomanian-Turonian strata of Western Carpathians enabled a complex study of ecological and geochemical proxies in relation to behavioural patterns of oyster Rhynchostreon suborbiculatum ...
Jakub Rantuch
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Global and Planetary Change, 2018
The Toarcian oceanic anoxic event (T-OAE; 183 Ma) was accompanied by severe biotic and geochemical perturbations that are considered as some of the most severe of the Mesozoic era.
G. Suan +6 more
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The Toarcian oceanic anoxic event (T-OAE; 183 Ma) was accompanied by severe biotic and geochemical perturbations that are considered as some of the most severe of the Mesozoic era.
G. Suan +6 more
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Tectonophysics, 1993
Abstract The Pieniny Klippen Belt represents a 600-km-long but only a few kilometers wide suture zone in the Carpathian orogenic belt. Based on a quantitative analysis along a part of its NW-trending segment in northeastern Slovakia, we present structural data supporting transpression, the continuous interaction of strike-slip shearing, horizontal ...
Lothar Ratschbacher +8 more
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Abstract The Pieniny Klippen Belt represents a 600-km-long but only a few kilometers wide suture zone in the Carpathian orogenic belt. Based on a quantitative analysis along a part of its NW-trending segment in northeastern Slovakia, we present structural data supporting transpression, the continuous interaction of strike-slip shearing, horizontal ...
Lothar Ratschbacher +8 more
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Cretaceous Research, 2008
Abstract This is a critical assessment of the paper by Oszczypko et al. (2004: Cretaceous Research 25, 89–113), in which they tried to prove a mid-Cretaceous age for the Szlachtowa (“black flysch”) and Opaleniec Formations, in the Pieniny Klippen Belt, West Carpathians, both of which had previously been shown to be of Jurassic age.
Krzysztof Birkenmajer +3 more
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Abstract This is a critical assessment of the paper by Oszczypko et al. (2004: Cretaceous Research 25, 89–113), in which they tried to prove a mid-Cretaceous age for the Szlachtowa (“black flysch”) and Opaleniec Formations, in the Pieniny Klippen Belt, West Carpathians, both of which had previously been shown to be of Jurassic age.
Krzysztof Birkenmajer +3 more
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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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Palaeogeography, Palaeoclimatology, Palaeoecology, 2011
Abstract The Bajocian and the Oxfordian–Kimmeridgian crinoidal limestones of the Pieniny Klippen Belt (PKB), Western Carpathians and the Bathonian–Callovian neptunian dykes which cut them were sampled for rock magnetic and palaeomagnetic study. The sampled sections were: Babina, Mestecko, Vrsatec, Bolesovska dolina and Szaflary.
M. Jeleńska, I. Túnyi, R. Aubrecht
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Abstract The Bajocian and the Oxfordian–Kimmeridgian crinoidal limestones of the Pieniny Klippen Belt (PKB), Western Carpathians and the Bathonian–Callovian neptunian dykes which cut them were sampled for rock magnetic and palaeomagnetic study. The sampled sections were: Babina, Mestecko, Vrsatec, Bolesovska dolina and Szaflary.
M. Jeleńska, I. Túnyi, R. Aubrecht
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Cretaceous Research, 1983
Abstract Eighteen Albian and Cenomanian planktic Foraminiferida from the Pieniny Klippen Belt of Poland are discussed. A local biostratigraphic zonation (six zones) is proposed and certain problems of palaeoecology are reviewed. The lithostratigraphical element is the so-called Trawne Beds, a Cretaceous flysch in the Pieniny Klippen Belt.
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Abstract Eighteen Albian and Cenomanian planktic Foraminiferida from the Pieniny Klippen Belt of Poland are discussed. A local biostratigraphic zonation (six zones) is proposed and certain problems of palaeoecology are reviewed. The lithostratigraphical element is the so-called Trawne Beds, a Cretaceous flysch in the Pieniny Klippen Belt.
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Geological Journal, 2018
Water temperature and productivity patterns during the middle Oxfordian through the late Kimmeridgian on the intrabasinal high in the Pieniny Basin, a part of the Western Tethys, have been identified by qualitative and quantitative analyses of ...
M. Bąk, K. Bąk
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Water temperature and productivity patterns during the middle Oxfordian through the late Kimmeridgian on the intrabasinal high in the Pieniny Basin, a part of the Western Tethys, have been identified by qualitative and quantitative analyses of ...
M. Bąk, K. Bąk
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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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