Central European Variscan Basement in the Outer Carpathians: A Case Study from the Magura Nappe, Outer Western Carpathians, Poland [PDF]
Minerals, 2021 Exotic crystalline blocks within the Outer Carpathian flysch have the potential to establish the nature of their eroded basement source(s) and thus to reconstruct the paleogeography of the Outer Carpathians. Petrological investigations (including mineral analyses) coupled with zircon and apatite U-Pb dating were performed on an exotic crystalline block
Aleksandra Gawęda +4 more
openaire +3 more sources
Acta Geologica Polonica, 2020 During the late Oligocene to early Miocene the residual Magura Basin was located along the front of the Pieniny Klippen Belt (PKB). This basin was supplied with clastic material derived from a south-eastern direction. In the Małe (Little) Pieniny Mts. in Poland, the late Oligocene/ early Miocene Kremna Fm.
Oszczypko, Nestor +2 more
openaire +2 more sources
Geologica Carpathica, 2015 Three small bodies of amphibolites and associated graphitic gneisses from the Suchý and Malá Magura Mountains (Tatric Megaunit, central Western Carpathians) have been studied by petrographic and geochemical methods.
Ivan Peter, Méres Štefan
doaj +1 more source
Trace element geochemistry of the Early to Late Cretaceous deposits of the Grajcarek thrust-sheets : a palaeoenvironmental approach (Małe Pieniny Mts., Pieniny Klippen Belt, Poland) [PDF]
, 2012 The chemical composition of the Cretaceous deposits of the Grajcarek thrust-sheets (Pieniny Klippen Belt, Poland) has been investigated to provide information on palaeoenvironment and provenance of pelagic and turbiditic particles.
Oszczypko, Nestor +1 more
core +1 more source
Veľké bentické dierkavce z eocénnych glaukonitových pieskovcov magurského príkrovu (Orava a Javorníky) [PDF]
Geologické práce. Správy, 2020 The aim of the work was to describe an assemblage of larger benthic foraminifers from quartz-glauconitic sandstones of the Bystrica Mb. of the Western Carpathian Magura Nappe.
Stanislav Buček, František Teťák
doaj
Geologica Carpathica, 2015 In this study, we revisit the stratigraphic age and discuss sedimentary characteristics of the lower Middle Jurassic turbidite deposits (“black flysch”) of the Szlachtowa Formation, as well as the under- and overlying members of the Sprzycne Creek ...
Segit Tomasz +2 more
doaj +1 more source
Paleogene of the Magura Nappe adjacent to the Pieniny Klippen Belt between Szczawnica and Krościenko (Outer Carpathians, Poland) [PDF]
Geology, Geophysics & Environment, 2014 The present authors investigated the Paleogene deposits of the internal zone of the Magura Basin known as Krynica Subunit or Krynica Zone in Poland. These deposits crop out in the peri-Pieniny zone, in area between Szczawnica and Krościenko. The oldest flysch deposits belong to the Paleocene – Lower Eocene Szczawnica Formation.
Jan Golonka, Anna Waśkowska-Oliwa
openaire +1 more source
The structural control of the Mroczna Cave development on the slopes of Mt Kornuty (the Flysch Carpathians, Beskid Niski Mts) [PDF]
, 2014 The Mroczna Cave is one of the longest caves in the Beskid Niski Mts., located on the south-western slopes of Mt Kornuty, along the main scarp of the landslide.
Zatorski, Michał
core +1 more source
The Beloveža Formation of the Rača Unit in the Beskid Niski Mts. (Magura Nappe, Polish Flysch Carpathians) and adjacent parts of Slovakia and their equivalents in the western part of the Magura Nappe; remarks on the Beloveža Formation – Hieroglyphic Beds [PDF]
Geological Quarterly, 2012 Eocene thin-bedded flysch, widespread in the Alpine Tethys ocean, is present within the Magura Nappe, the largest Outer Carpathian unit in Poland and Slovakia. Thin-bedded flysch sedimentation accompanied by hemipelagic shales took place accross the entire Magura Basin during Eocene times.
Jan Golonka, Anna Waśkowska
openaire +1 more source
Early Cretaceous intra-plate volcanism in the Pieniny Klippen Belt : a case study of the Velykyi Kamenets'/Vilkhivchyk (Ukraine) and Biała Woda (Poland) sections [PDF]
, 2012 The geological position and geochemistry of the basaltic sill and tuffs occurring within the Berriasian-?Albian pelagic limestones of the Czorsztyn Succession are described.
Krobicki, Michał +2 more
core +1 more source