Results 191 to 200 of about 7,206 (227)
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2009
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, MICHELE +4 more
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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, MICHELE +4 more
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2020
<p>Located in northern Morocco, the Rif belt represents the western edge of the Maghrebides system. This domain underwent a significant Cenozoic alpine compressional deformation, due to the collision between the North African margin and the south-western margin of the exotic Alboran Domain.
Andrea Schito +5 more
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<p>Located in northern Morocco, the Rif belt represents the western edge of the Maghrebides system. This domain underwent a significant Cenozoic alpine compressional deformation, due to the collision between the North African margin and the south-western margin of the exotic Alboran Domain.
Andrea Schito +5 more
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Sedimentary Geology, 1985
Abstract The magnetic fabric of sandstone of the Ždanice-Hustopece Formation (Flysch Belt of the West Carpathians) is essentially sedimentary in origin, although affected very weakly by ductile deformation. The magnetic lineation is mostly parallel to the flow direction.
František Hrouda, Zdeněk Stráník
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Abstract The magnetic fabric of sandstone of the Ždanice-Hustopece Formation (Flysch Belt of the West Carpathians) is essentially sedimentary in origin, although affected very weakly by ductile deformation. The magnetic lineation is mostly parallel to the flow direction.
František Hrouda, Zdeněk Stráník
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2015
The paper summarizes results of both empirical and modelling research of bedload transport in headwater streams of the Czech part of the Western Carpathians. Flysch lithology (i.e. alternation of less resistant claystones and sandstones) affects bedload transport parameters in view of relatively fine-sized sediment supply resulting in low flow ...
Tomáš Galia +2 more
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The paper summarizes results of both empirical and modelling research of bedload transport in headwater streams of the Czech part of the Western Carpathians. Flysch lithology (i.e. alternation of less resistant claystones and sandstones) affects bedload transport parameters in view of relatively fine-sized sediment supply resulting in low flow ...
Tomáš Galia +2 more
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AAPG Bulletin, 1988
In the abstract by Charles A. Ferguson and Neil H. Suneson, entitled "Arbuckle source for Atoka Formation Flysch, Ouachita Mountains Frontal Belt, Oklahoma: New Evidence for Paleocurrents" (AAPG Bulletin, v. 72, p. 184-185), the final sentence of the second paragraph should read, "The bounding faults would be the southernmost of a series of northward ...
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In the abstract by Charles A. Ferguson and Neil H. Suneson, entitled "Arbuckle source for Atoka Formation Flysch, Ouachita Mountains Frontal Belt, Oklahoma: New Evidence for Paleocurrents" (AAPG Bulletin, v. 72, p. 184-185), the final sentence of the second paragraph should read, "The bounding faults would be the southernmost of a series of northward ...
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Acta Geologica Sinica - English Edition, 1999
Abstract Twenty‐three ichnotaxa have been found in the Silurian and Carboniferous turbidites of the Tianshan orogenic belt and the Triassic turbidites of the East Kunlun‐West Qinling orogenic belt of northwestern China. They are Acanthorhaphe isp., ?Arthrophycus isp., Aulichnites parkerensis, Chondrites isp., C. intricatus, C.
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Abstract Twenty‐three ichnotaxa have been found in the Silurian and Carboniferous turbidites of the Tianshan orogenic belt and the Triassic turbidites of the East Kunlun‐West Qinling orogenic belt of northwestern China. They are Acanthorhaphe isp., ?Arthrophycus isp., Aulichnites parkerensis, Chondrites isp., C. intricatus, C.
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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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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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Arabian Journal of Geosciences, 2018
The Zoumi Basin was generated in a collisional tectonic setting during the Lower-Middle Miocene. The syn-orogenic flysch deposits of the basin have been well investigated by petrographic and geochemical studies to characterize the composition, source to sink routing system, and tectonic setting of the Zoumi flysch.
Mohamed El Mourabet +4 more
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The Zoumi Basin was generated in a collisional tectonic setting during the Lower-Middle Miocene. The syn-orogenic flysch deposits of the basin have been well investigated by petrographic and geochemical studies to characterize the composition, source to sink routing system, and tectonic setting of the Zoumi flysch.
Mohamed El Mourabet +4 more
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Limestone Klippen Belt—Atypical Landforms in Flysch Uplands
2022Dušan Plašienka, Ján Novotný
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