Results 21 to 30 of about 259 (94)

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
Szczęch, Mateusz, Waśkowska, Anna
openaire   +3 more sources

The Lower Miocene deposits of the Rača Subunit near Nowy Sącz (Magura Nappe, Polish outer Carpathians)

, 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, Andreyeva-Grigorovich, Aida S., Malata, Ewa, Oszczypko-Clowes, Marta   +3 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, Leszczyński, Stanisław   +1 more
openaire   +2 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, Oszczypko, Nestor   +1 more
openaire   +2 more sources

A wealth of P–T–t information from metasediments in the HP–UHP terrane of the Pohorje Mountains, Slovenia, elucidates the evolution of the Eastern Alps

Journal of Metamorphic Geology, Volume 41, Issue 9, Page 1167-1196, December 2023., 2023
Abstract Contrasting views exist in regard of the evolution of metamorphic rocks in the southeastern Pohorje Mountains (Mts), located in the southeastern Eastern Alps. Major debated points are whether micaschists have experienced ultrahigh‐pressure metamorphism in the Late Cretaceous (Eo‐Alpine) and whether they were continuously exhumed or experienced
Botao Li, Hans‐Joachim Massonne, Xiaoping Yuan   +2 more
wiley   +1 more source

Isolating Lithologic Versus Tectonic Signals of River Profiles to Test Orogenic Models for the Eastern and Southeastern Carpathians

Journal of Geophysical Research: Earth Surface, Volume 126, Issue 8, August 2021., 2021
Abstract Fluvial morphology is affected by a wide range of forcing factors, which can be external, such as faulting and changes in climate, or internal, such as variations in rock hardness or degree of fracturing. It is a challenge to separate internal and external forcing factors when they are co‐located or occur coevally.
B. Gailleton, H. D. Sinclair, S. M. Mudd, E. L. S. Graf, L. C. Mațenco   +4 more
wiley   +1 more source

The Upper Cretaceous variegated shales in the Ropianka Formation of the Magura Nappe (Outer Carpathians) – age and lithostratigraphic position

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

Comparison analysis of numerically calculated slip surfaces with measured S-wave velocity field for Just-Tęgoborze landslide in Carpathian flysch [PDF]

E3S Web of Conferences, 2019
The article presents the comparison analysis between deformation field from numerical model and shear wave (S-wave) velocity field obtained from seismic interferometry (SI). Tests were conducted on active Just-Tęgoborze landslide. Geologically, the study
Krawiec Krzysztof, Harba Paulina
doaj   +1 more source

Biostratigraphic constraints for a Lutetian age of the Harrersdorf Unit (Rhenodanubian Zone): Implication for basement structure of the northern Vienna Basin (Austria)

Geologica Carpathica, 2019
The formations underlying the Neogene infill of the Vienna Basin are still poorly documented. Until now correlation of subsurface lithostratigraphic units with those of the Rhenodanubian nappe system and the Magura nappe system, outcropping at the basin ...
Kranner Matthias, Harzhauser Mathias, Rögl Fred, Ćorić Stjepan, Strauss Philipp   +4 more
doaj   +1 more source

An integrated paleomagnetic and magnetic anisotropy study of the Oligocene flysch from the Dukla nappe, Outer Western Carpathians, Poland

Geologica Carpathica, 2016
The Dukla Nappe belongs to the Outer Western Carpathians, which suffered considerable shortening due to the convergence and collision of the European and African plates.
Kiss Dániel, Márton Emő, Tokarski Antek K.   +2 more
doaj   +1 more source