Foraminifera from the Eocene Variegated Shales near Barwinek (Magura Unit, Outer Carpathians), the type locality of Noth (1912) revisited [PDF]
, 2005 Kaminski, MA, Cieszkowski, M, Kender, S
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Poręba Wielka : small-scale faulting in the Rača and Bystrica slices of the Magura Nappe
, 2001 openaire +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 Waskowska
exaly +4 more sources
Stratigraphy and Geological Structure of the Magura Nappe in the South-Western Part of the Gorce Mountains, Outer Carpathians, Poland [PDF]
Annales Societatis Geologorum Poloniae, 2023 The south-western part of the Gorce Mts (Outer Carpathians) is composed of flysch deposits of the Krynica and Bystrica subunits of the Magura Nappe. The Krynica Subunit includes the Late Cretaceous–Paleocene Ropianka Fm, the Early Eocene Beloveža Fm, the
Mateusz Szczech, Anna Waskowska
exaly +5 more sources
Early Miocene Age of the Stare Bystre Formation Based on Calcareous Nannofossils (Magura Nappe, Outer Carpathians, Poland) [PDF]
Geological Quarterly, 2016 The area of investigation is situated close to the contact zone between the Pieniny Klippen Belt, Krynica Subunit of the Magura Nappe and the Neogene strata of the Orava–Nowy Targ Intramontane Basin (southern Poland). In the area studied, marine deposits of the Stare Bystre Formation outcrop at the surface where they emerge from beneath freshwater and ...
Marta Oszczypko-Clowes +1 more
exaly +6 more sources
Geological Setting and Lithological Inventory of the Czarna Woda Conglomerates (Magura Nappe, Polish Outer Carpathians) [PDF]
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
exaly +5 more sources