Abstract The magnetic fabric of sandstones in thrust sheets of the Flysch Belt of the Western Carpathians is basically sedimentary in origin, in minority of specimens slightly affected by deformation which is generally very weak, corresponding to the earliest deformation stage and to Types I-II in terms of the magnetic fabric classification of the ...
František Hrouda
exaly +2 more sources
Abstract Landslides are important geomorphic agents in various mountainous settings. We document here a case of river piracy from the upper part of the Mala Brodska Valley in the Vsetinske Mts., Czech Republic (Raca Unit of the flysch Magura Group of Nappes, flysch belt of the Outer Western Carpathians) controlled by mass movement processes. Based on
Ivo Baron, Michal Bil, Ondřej Babek
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Limestone Klippen Belt—Atypical Landforms in Flysch Uplands
World Geomorphological Landscapes, 2022Dusan Plašienka, Jan Novotny
exaly +2 more sources
Ophiolite-bearing vermoshi flysch (Albanian alps, Northern Albania): Elements for its correlation in the frame of dinaric-hellenic belt [PDF]
The tectonic setting of the Albanian Alps, Northern Albania, is characterized by a thick pile of tectonic units whose uppermost structural level is represented by the Vermoshi Unit, cropping out just few km north of the Shkoder-Péc Line. This unit includes a single formation, the Vermoshi Flysch, characterized by turbidite deposits consisting of ...
Marroni M +4 more
core +4 more sources
Mississippian synorogenic sedimentation in the Variscan belt: Why are NW and SW Iberia flysch basins so different and yet so similar? [PDF]
Devonian-Carboniferous synorogenic sedimentation is described across the Variscan orogen, as well-preserved exposures in late orogenic structures between continental blocks. Variscan marine sedimentary sequences are described in both colliding continents: Gondwana representative of the southern subducting super-plate, and Laurussia considered as the ...
Ícaro Dias da Silva +2 more
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A constrained African craton source for the Cenozoic Numidian Flysch: Implications for the palaeogeography of the western Mediterranean basin [PDF]
The provenance of the Numidian Flysch in the western Mediterranean remains a controversial subject which hinders understanding of this regionally widespread depositional system. The Numidian Flysch is a deep marine formation dated as Oligocene to Miocene
M F H Thomas, Stéphane Bodin
exaly +2 more sources
Role of flysch in rock avalanches formation in the eastern sector of the Alpine-Mediterranean belt
Role of flysch in rock avalanches formation in the eastern sector of the Alpine-Mediterranean belt, 2022Ruolo del flysch nella formazione di valanghe di roccia nel settore orientale della catena Alpino-Mediterranea Il flysch è una delle successioni sedimentarie sinorogeniche più diffuse nel mondo, caratterizzata da sedimentazione ciclica e variabilità significativa delle proprietà meccaniche che risultano complessivamente modeste.
Strom, Alexander, Zerkal, Oleg
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Burial and thermal history of the Carpathian flysch belt in the Eastern Moravia Czech Republic
Proceedings, 1996The hydrocarbon potential of the Flysch Belt of the West Carpathians has been studied using source rock geochemistry and basin modeling. A geodynamic model is proposed for the region of the Eastern Czech republic showing key points in the Flysch basins and overthrust evolution, The term Flysch is used here for tectonic units which comprise not only ...
J. Francu +3 more
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New Oil Exploration Results in the Flysch Belt, the West Carpathians, Slovakia
61st EAGE Conference and Exhibition, 1999Renewed interest on oil exploration in the Flysch Belt of the West Carpathians in the Slovak Republic (Fig.1) results from a revaluation of older exploration work, organic geochemical investigation of potential source rocks and surface shows of hydrocarbons.
J. Zelman +3 more
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Out-of-sequence thrusts and paleogeography of the Rhenodanubian Flysch Belt (Eastern Alps) revisited
International Journal of Earth Sciences, 2007The Oberstdorf nappe of the Western and the Laab nappe of the Eastern Rhenodanubian Flysch (ERF) were independently identified as out-of-sequence thrust units by facies studies (Mattern 1999) and zircon analyses (Trautwein et al. 2001a, b, c), respectively.
Frank Mattern, Pu Jun Wang
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