Results 21 to 30 of about 19,531 (99)
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
doaj +3 more sources
The position and age of the youngest deposits in the Mszana Dolna and Szczawa tectonic windows (Magura Nappe, Western Carpathians, Poland) [PDF]
, 2004 The Mszana Dolna and Szczawa tectonic windows are composed of deposits belonging to the Fore-Magura Group of units. The central and most uplifted part of these windows are dominated by relatively flat laying deposits belonging to the Krosno Formation (Oligocene) of the Dukla Unit.
Oszczypko-Clowes, Marta +1 more
openaire +2 more sources
Palynology of the Eocene-Oligocene transition in the marginal zone of the Magura Nappe at Folusz (Western Carpathians, Poland) [PDF]
, 2005 Palynological investigations of the deep-marine Upper Eocene-Lower Oligocene, mainly turbiditic andhemipelagic sediments exposed at Folusz (Siary Zone of Magura Nappe, Polish part of the Western Carpathians), revealed a prevalence of land plant remains in the palynofacies. Dinoflagellate cysts are the most frequent among marine palynomorphs.
Gedl, Przemysław +1 more
openaire +2 more sources
, 1999 In the area of Nowy Sącz the Lower Miocene, marine deposits (of the N 5, NN 2-3 biozones) have been discovered in the southern part of the Rača Subunit of the Magura Nappe. These deposits belong to the Zawada Fm., which probably overlaps the Malcov Fm. (Upper Eocene-Oligocene) with an erosional hiatus.
Oszczypko, Nestor +3 more
openaire +2 more sources
Geological Quarterly, 2023 The lithological characteristics and age analysis of the variegated Farony Shale are presented for the first time. The Farony Shale occurs in the Lubomierz and Rabka areas in the Bystrica Subunit. It is located within medium- and thin-bedded sandy dominated turbidites of the Campanian–Paleocene Ropianka Formation.
Waśkowska, Anna, Szczęch, Mateusz
openaire +2 more sources
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
Geologické práce. SprávyThe work presents maps of the selected regions of the western Slovak section of the Flysch Belt of the Western Carpathians, including the contact with the Klippen Belt, compiled by the author in the period from 2001 to 2023.
František Teťák
doaj +1 more source
EnergiesThe paper presents the geochemical characteristics of 26 selected oil seeps, more than half of which are remnants of old oil wells. The samples were collected from three tectonic units: the Magura, Silesian, and Skole units in the Polish part of the ...
Wojciech Bieleń +3 more
doaj +1 more source
The stratigraphy of the Ropa tectonic window (Magura Nappe, Western Carpathians, Poland) [PDF]
, 2008 The Ropa tectonic window of the Magura Nappe is composed of Oligocene deposits that belong to the Grybów Nappe. The youn gest depos its of the Ropa tectonic window are correlated with calcareous nannoplanton zones NP24 and NP25.
Oszczypko-Clowes, Marta
core
Tectonics, Volume 45, Issue 10, October 2026.Abstract Following continental collision, the distal European margin was overridden by the Alpine wedge and is now largely concealed beneath the mostly intact orogenic lid. Consequently, the geological evolution and nature of the hidden basement domains remain poorly constrained.
Bianca Heberer +11 more
wiley +1 more source