Results 161 to 170 of about 831 (199)
The raising and westward expansion of central Tibet. [PDF]
Natl Sci RevZhao C +15 more
europepmc +1 more source
New faunistic records of chironomids and phantom midges (Diptera, Chironomidae and Chaoboridae) from Ukraine indicate recent climatic refugia in the Eastern Carpathians. [PDF]
ZookeysBitušík P +3 more
europepmc +1 more source
Soil erosion susceptibility assessment in the Bistrița River basin (Romania) using machine learning algorithms and GIS. [PDF]
Sci RepMuratoreanu G +8 more
europepmc +1 more source
Canadian Journal of Earth Sciences, 1980 An Ordovician flysch trace fossil assemblage from the Aroostook–Matapedia Carbonate Belt, northern New Brunswick, consists of the following identifiable ichnogenera: Alcyonidiopsis, Asteriacites, Asterosoma, Belorhaphe, Bifasciculus, Buthotrephis, Chondrites, Cochlichnus, Cosmorhaphe, Diplichnites, Fucusopsis, Glockeria, Gyrochorte, Helminthoida ...
R K Pickerill
exaly +3 more sources
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Pure and Applied Geophysics, 2018
The paper presents the interpretation of magnetotelluric measurements along the SW–NE profile near Stara Ľubovňa (Northern Slovakia). The profile passes through the Outer Carpathian Flysch Belt, Klippen Belt and ends in the Inner Western Carpathians Paleogene NW from Ružbachy horst structure.
Dusan Majcin +2 more
exaly +2 more sources
The paper presents the interpretation of magnetotelluric measurements along the SW–NE profile near Stara Ľubovňa (Northern Slovakia). The profile passes through the Outer Carpathian Flysch Belt, Klippen Belt and ends in the Inner Western Carpathians Paleogene NW from Ružbachy horst structure.
Dusan Majcin +2 more
exaly +2 more sources
Cretaceous Research, 2008
Abstract This is a critical assessment of the paper by Oszczypko et al. (2004: Cretaceous Research 25, 89–113), in which they tried to prove a mid-Cretaceous age for the Szlachtowa (“black flysch”) and Opaleniec Formations, in the Pieniny Klippen Belt, West Carpathians, both of which had previously been shown to be of Jurassic age.
Jarosław Tyszka
exaly +2 more sources
Abstract This is a critical assessment of the paper by Oszczypko et al. (2004: Cretaceous Research 25, 89–113), in which they tried to prove a mid-Cretaceous age for the Szlachtowa (“black flysch”) and Opaleniec Formations, in the Pieniny Klippen Belt, West Carpathians, both of which had previously been shown to be of Jurassic age.
Jarosław Tyszka
exaly +2 more sources
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
exaly +2 more sources
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
exaly +2 more sources
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
exaly +2 more sources
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 ...
Jan Lenart +2 more
exaly +3 more sources
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 ...
Jan Lenart +2 more
exaly +3 more sources
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
exaly +2 more sources
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
exaly +2 more sources