Field trip – Outer Flysch Carpathians and Pieniny Klippen Belt (PKB) [PDF]
Geotourism/Geoturystyka, 2023 We are glad that we can meet personally during the 2nd Symposium of the IGCP 710 Project, after the pandemic time, which disrupted our idea of regular, annual meetings.
Krobicki (ed.), Michał
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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.
Golonka, Jan +2 more
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THE PIENINY KLIPPEN BELT: ITS TECTONIC STRUCTURE AND EVOLUTION
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
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DEEP WATER AGGLUTINATED FORAMINIFERA FROM THE JURASSIC/CRETACEOUS BOUNDARY AND PALEOENVIRONMENTAL SETTINGS OF THE MAIOLICA TYPE FACIES FROM THE CZORSTYN RIDGE (PIENINY KLIPPEN BELT, WESTERN CARPATHIANS) [PDF]
Rivista Italiana di Paleontologia e Stratigrafia, 2017 Deep-water carbonates deposited on the Czorstyn elevated ridge of the Pieniny Klippen Belt paleogeographic domain record changes in agglutinated foraminifera morphogroups through the J/K boundary interval at the Erdútsky kostol section.
ŠTEFAN JÓZSA
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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 +5 more
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EARLY TITHONIAN DEEP-WATER COLONIZATION BY BENTHIC FORAMINIFERA IN THE MAGURA BASIN (PIENINY KLIPPEN BELT, WESTERN CARPATHIANS): A CLUE TO THE ORIGINS OF DEEP-WATER FORAMINIFERA. [PDF]
Rivista Italiana di Paleontologia e Stratigrafia, 2019 Deep-water benthic foraminifera were reported from lower Tithonian abyssal deposits lying above a barren interval of radiolarites in the Magura Basin (Western Carpathians).
ŠTEFAN JÓZSA
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JURASSIC PALEOGEOGRAPHY OF THE PIENINY AND OUTER CARPATHIAN BASINS [PDF]
Rivista Italiana di Paleontologia e Stratigrafia, 2004 The Jurassic history of the Pieniny/Outer Carpathian basins reflects the evolution of the Circum-Tethyan area, especially its Alpine Tethys part. The Alpine Tethys that is Ligurian, Penninic Oceans and Pieniny/Magura Basin constitute the extension of the
JAN GOLONKA, MICHAL KROBICKI
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Age and provenance of mica-schist pebbles from the Eocene conglomerates of the Tylicz and Krynica Zone (Magura Nappe, Outer Flysch Carpathians) [PDF]
Geologica Carpathica, 2016 During the Łate Cretaceous to Palaeogene, the Magura Basin was supplied by clastic material from source areas situated on the northern and southern margins of the basin, which do not outcrop on the surface at present.
Oszczypko Nestor +2 more
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MineralogiaVolcanic rocks in the Pieniny Klippen Belt (PKB) of the Western Carpathians have been the focus of geologists for over a century (e.g. Uhlig, 1890; Małkowski, 1921). Miocene volcanism is most common in the PKB.
Bazarnik Jakub +5 more
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Upper Jurassic shallow-water scleractinian corals from the Pieniny Klippen Belt (Western Carpathians, Slovakia) [PDF]
, 2005 Oxfordian shallow-water scleractinian coral association from the biohermal limestones of the Mt Vršatec (Czorsztyn Succession, Slovak sector of the Pieniny Klippen Belt, Western Carpathians) comprises 18 species (among them 2 new) plus 3 taxa determined
Mišík, Milan, Morycowa, Elżbieta
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