Results 1 to 10 of about 589 (75)

Structure and dynamics of deep-seated slope failures in the Magura Flysch Nappe, outer Western Carpathians (Czech Republic) [PDF]

Natural Hazards and Earth System Sciences, 2004
Deep-seated mass movements currently comprise one of the main morphogenetic processes in the Flysch Belt of the Western Carpathians of Central Europe. These mass movements result in a large spectrum of slope failures, depending on the type of movement ...
I. Baron, I. Baron, V. Cilek, O. Krejci, R. Melichar, F. Hubatka   +5 more
doaj   +3 more sources

Numerical analysis of deep-seated mass movements in the Magura Nappe; Flysch Belt of the Western Carpathians (Czech Republic) [PDF]

Natural Hazards and Earth System Sciences, 2005
Deep-seated slope failures are common features in the mountains of the Raca Unit, Magura Nappe of the Flysch Belt of Western Carpathians. Since they represent very complicated system, understanding of their evolution and triggers still remains unclear ...
I. Baron, I. Baron, F. Agliardi, C. Ambrosi, G. B. Crosta   +4 more
doaj   +3 more sources

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, Salata Dorota, Konečný Patrik   +2 more
doaj   +3 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

Geology of the Magura Nappe, south-western Gorce Mountains (Outer Carpathians, Poland)

Journal of Maps, 2021
The studied area, located in the south-western part of the Gorce Mountains, is built of flysch deposits representing the Krynica and Bystrica Subunits of the Magura Nappe.
Mateusz Szczęch, Marek Cieszkowski
doaj   +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

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

Geological structure and evolution of the Pieniny Klippen Belt to the east of the Dunajec River : a new approach (Western Outer Carpathians, Poland) [PDF]

, 2014
The area studied, known as the Małe (Little) Pieniny Mts., belongs to the Pieniny Klippen Belt (PKB), a suture zone that separates the Central Carpathians from the Outer Carpathian accretionary wedge. Along its northern boundary the PKB is separated from
Oszczypko, Nestor, Oszczypko-Clowes, Marta   +1 more
core   +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