Results 121 to 130 of about 190,285 (154)
Some of the next articles are maybe not open access.
Late Cretaceous deformation of the Pieniny Klippen Belt, West Carpathians
Tectonophysics, 1994Abstract The Late Cretaceous position and dynamics of the Pieniny Klippen Belt of the West Carpathians, which lies behind the Palaeogene flysch accretionary prism, are reconstructed. As shown by the reconstruction, based on structural, sedimentological and palaeomagnetic data, the Pieniny Klippen Belt occupied a WNW-ESE to NW-SE trending zone during ...
M. Nemcok, J. Nemcok
exaly +2 more sources
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.
Jarosław Tyszka
exaly +2 more sources
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.
Jarosław Tyszka
exaly +2 more sources
International Journal of Earth Sciences, 2019
The Pieniny Klippen Belt (PKB) and adjoining zones form a narrow, but lengthy belt that separates the Cretaceous nappe stack of the Central (Austroalpine) and the Cenozoic accretionary wedge of the External Western Carpathians (Flysch Belt). The PKB shares units and structures of both, in addition to the distinctive Oravic units, derived from a ...
Dušan Plašienka +2 more
openaire +2 more sources
The Pieniny Klippen Belt (PKB) and adjoining zones form a narrow, but lengthy belt that separates the Cretaceous nappe stack of the Central (Austroalpine) and the Cenozoic accretionary wedge of the External Western Carpathians (Flysch Belt). The PKB shares units and structures of both, in addition to the distinctive Oravic units, derived from a ...
Dušan Plašienka +2 more
openaire +2 more sources
SCIENTIFIC PAPERS OF DONNTU Series: “The Mining and Geology”, 2023
Purpose. Micropaleontological characteristics of individual exposed sections of Turonian-Maastrichtian sediments of the Pieniny Klippen Belt in the Ukrainian Carpathians with detailed age determination by foraminifera. Method. Field geological and stratigraphic research, foraminiferal analysis. Results.
K. Navarivska
openaire +2 more sources
Purpose. Micropaleontological characteristics of individual exposed sections of Turonian-Maastrichtian sediments of the Pieniny Klippen Belt in the Ukrainian Carpathians with detailed age determination by foraminifera. Method. Field geological and stratigraphic research, foraminiferal analysis. Results.
K. Navarivska
openaire +2 more sources
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 +2 more
exaly +2 more sources
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 +2 more
exaly +2 more sources
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.
exaly +2 more sources
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.
exaly +2 more sources
Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen
Christian Meister +5 more
openaire +2 more sources
Christian Meister +5 more
openaire +2 more sources