Results 1 to 10 of about 50 (47)
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 Szczech, Marek Cieszkowski
exaly +2 more sources
Alternative Interpretation of the Bystrica Unit in Klanečnica KLK-1 Borehole (Magura Nappe)
Mineralia SlovacaIn 1986, the KLK-1 (Klanečnica) borehole was drilled northwest of Moravské Lieskové as part of a regional oil and gas exploration programme. The well reached a total depth of 662 m and was intended to verify the occurrence and potential accumulation of ...
František Teťák +2 more
exaly +3 more sources
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 ...
Ivo Baroň, Rostislav Melichar
exaly +1 more source
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 +2 more
wiley +1 more source
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 +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
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 +4 more
doaj +1 more source
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 +2 more
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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
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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