Results 11 to 20 of about 190,285 (154)

THE PIENINY KLIPPEN BELT: ITS TECTONIC STRUCTURE AND EVOLUTION [PDF]

Геодинамика и тектонофизика, 2015
Many mobile belts contain narrow (a few kilometres wide) and elongated (several hundreds and thousands kilometres long) zones characterized by complicated tectonic interiors and intensive rock metamorphism.
M. G. Leonov
doaj   +4 more sources

Kinematic evolution of the Pieniny Klippen Belt in Cenozoic (Ukrainian Carpathians)

Геофизический журнал, 2016
The data on surface, subsurface and deep structure of the Pieniny Klippen Belt (PKB) have been summarized and new results of its geological-structural and fault kinematic studies within the Ukrainian part of the Eastern Carpathians have been presented ...
A. V. Murovskaya, M. V. Nakapelyukh, Yu. M. Vikhot, V. E. Shlapinskiy, I. N. Bubnyak, S. V. Mychak   +5 more
doaj   +5 more sources

The Pieniny Klippen Belt in Poland [PDF]

Geology, Geophysics & Environment, 2018
The Pieniny Klippen Belt in Poland marks the Central Carpathian-North European plate suture zone. The strictly tectonic present-day confines of the Pieniny Klippen Belt are characterized as (sub)vertical faults and shear zones. A strong reduction in the space of the original sedimentary basins took place. The strike-slip-bounded tectonic blocks, thrust
Jan Golonka, Michał Krobicki, Anna Waśkowska   +2 more
semanticscholar   +5 more sources

Aptian age of the “spotted limestone” (Pieniny Limestone Formation) in Grajcarek Stream (Pieniny Klippen Belt, Poland) [PDF]

Annales Societatis Geologorum Poloniae, 2015
Planktonic foraminifera, calcareous dinocysts and nannofossils have been identified in thin sections of the “spotted limestone”, exposed in the Grajcarek Stream at Szlachtowa and assigned to the Pieniny Limestone Formation in the Magura Succession, Pieniny Klippen Belt (southern Poland).
Wójcik-Tabol, Patrycja, Oszczypko, Nestor   +1 more
semanticscholar   +8 more sources

Santonian-Campanian marly and biodetritic facies in the Púchov Formation in the Orava sector of the Pieniny Klippen Belt (Slovakia)

Mineralia Slovaca
The Pieniny Klippen Belt is characterized by the block-in-matrix fabric with Jurassic to Lower Cretaceous rigid klippen embedded in less competent Upper Cretaceous flysch and marlstone matrix.
Ondrej Pelech, Štefan Józsa, Mário Olšavský   +2 more
doaj   +2 more sources

Thermal Maturity of the Grajcarek Unit (Pieniny Klippen Belt): Insights for the Burial History of a Major Tectonic Boundary of the Western Carpathians

Minerals (Basel, Switzerland), 2021
The Grajcarek Unit of the Pieniny Klippen Belt (PKB), at the boundary between the Central (Inner) and Outer Carpathians, resulted from the convergence of the ALCAPA (the Alps–Carpathians–Pannonia) block and European plate. The strongly deformed slices of
Magdalena Zielinska
exaly   +2 more sources

Heavy mineral analysis of the Upper Cretaceous to Lower Eocene synorogenic formations of the Pieniny Klippen Belt (Šariš Unit, eastern Slovakia): new data from the Jar-2 borehole (Jarmuta-Proč Fm.) and outcrops (Malinowa Fm.)

Mineralia Slovaca
The study presents new results of heavy mineral analyses including detrital garnet, tourmaline and Cr-rich spinel chemical compositions from the synorogenic Maastrichtian-Ypresian Jarmuta-Proč Fm. of the Šariš Unit of the Pieniny Klippen Belt, penetrated
Jozef Madzin, Dušan Plašienka
doaj   +2 more sources

Revisiting the Age of Jurassic Coral Bioherms in the Pieniny Klippen Belt (Western Carpathians) on the Basis of Benthic Foraminifers

Geologica Carpathica, 2019
Coral bioherms of the Vršatec Limestone that formed massive, several tens of meters thick complexes during the Jurassic were important sources of carbonate production, with carbonate sediment exported to deeper parts of the Pieniny Klippen Basin (Western
Ivanova Daria K., Schlögl Ján, Tomašových Adam, Lathuilière Bernard, Golej Marián   +4 more
doaj   +2 more sources

Provenance of synorogenic deposits of the Upper Cretaceous–Lower Palaeogene Jarmuta–Proč Formation (Pieniny Klippen Belt, Western Carpathians)

Geologica Carpathica, 2019
The Pieniny Klippen Belt contains thickening and coarsening upwards synorogenic sedimentary successions witnessing the collision of the Oravic ribbon continent with the Central Carpathian orogenic wedge after the closure of the Vahic Ocean in the Late ...
Madzin Jozef, Plašienka Dušan, Méres Štefan   +2 more
doaj   +2 more sources

The Šariš Transitional Zone, revealing interactions between Pieniny Klippen Belt, Outer Carpathians and European platform

Swiss Journal of Geosciences, 2018
The Pieniny Klippen Belt (PKB) is a narrow structure delineating the boundary between the Central and Outer Carpathians. It is built of nappes stacked during the Cretaceous and Paleocene and then re-folded in the Miocene during the formation of the Outer
Edyta Jurewicz
exaly   +2 more sources