Results 181 to 190 of about 7,213 (219)
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Tectonophysics, 2009
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 +3 more
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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 +3 more
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Geomorphology, 2014
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 Baroň +5 more
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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 Baroň +5 more
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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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Outline of Petroleum Geology of the Flysch Belt, West Carpathians, Slovakia
60th EAGE Conference and Exhibition, 1998Petroleum geological field research has for a long duration showed occurrences of hydrocarbons in the West Carpathian Flysch Belt (Fig. 1).
M. Pereszlény, J. Milicka, R. Vitálos
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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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Internal structure and main evolution phases of the Flysch Belt, Carpathians, Czech Republic
Proceedings, 1996The Flysch Belt of the West Carpathians in the eastern Czech Republic is a nappe complex formed by the polyphase Neoalpine orogeny during the Late Paleogene and Early Miocene. Based on lithofacies and tectonics the Flysch Belt is subdivided into the Krosno -Menilite- and Magura Groups of nappes.
O. Krejcl +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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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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Geology, 1996
During the Cambrian-Ordovician the paleo–Pacific margin of Gondwana underwent a rapid transition from a site of convergent deformation (Delamerian-Ross orogeny) to one of sedimentation during which the thick turbiditic sequences of the adjacent basal Lachlan fold belt were deposited. Laser-probe 40 Ar- 39 Ar data show that the synkinematic (523–486 Ma)
Turner, S. +5 more
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During the Cambrian-Ordovician the paleo–Pacific margin of Gondwana underwent a rapid transition from a site of convergent deformation (Delamerian-Ross orogeny) to one of sedimentation during which the thick turbiditic sequences of the adjacent basal Lachlan fold belt were deposited. Laser-probe 40 Ar- 39 Ar data show that the synkinematic (523–486 Ma)
Turner, S. +5 more
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Precambrian Research, 1982
Abstract The Granulite belt of Lapland comprises two main units. The more extensive unit, the khondalite suite, is formed of approximately equal proportions of sillimanite-garnet gneisses and garnet gneisses which include impersistent layers of quartz-rich gneisses, calc-silicate rocks and metavolcanics.
P BARBEY, R CAPDEVILA, J HAMEURT
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Abstract The Granulite belt of Lapland comprises two main units. The more extensive unit, the khondalite suite, is formed of approximately equal proportions of sillimanite-garnet gneisses and garnet gneisses which include impersistent layers of quartz-rich gneisses, calc-silicate rocks and metavolcanics.
P BARBEY, R CAPDEVILA, J HAMEURT
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