Results 191 to 200 of about 7,213 (219)
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Geomorphology, 2014
Abstract Crevice-type caves are among the least investigated natural phenomena connected with the development of slope failures. These caves present complex and peculiar underground systems with their own development and resulting landforms. We investigated eight caves in the Czech part of the Outer Western Carpathians to determine their genesis ...
Lenart, Jan +2 more
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Abstract Crevice-type caves are among the least investigated natural phenomena connected with the development of slope failures. These caves present complex and peculiar underground systems with their own development and resulting landforms. We investigated eight caves in the Czech part of the Outer Western Carpathians to determine their genesis ...
Lenart, Jan +2 more
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2023
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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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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2006
For the identification of the North European platform below the Western Carpathian Flysch belt and for the definition of the lithospheric and crustal relationships in the collisional zone between the Western Carpathian block and the North European platform, two migrated reflection seismic profiles with deep registration were chosen in the eastern ...
Igor Hrušecký +2 more
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For the identification of the North European platform below the Western Carpathian Flysch belt and for the definition of the lithospheric and crustal relationships in the collisional zone between the Western Carpathian block and the North European platform, two migrated reflection seismic profiles with deep registration were chosen in the eastern ...
Igor Hrušecký +2 more
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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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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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