Results 171 to 180 of about 7,213 (219)
Constraints on ore vectoring from geochemical fingerprints of porphyry style pyrite. [PDF]
Naglik B +10 more
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Projecting Extinction Risk and Assessing Conservation Effectiveness for Three Threatened Relict Ferns in the Western Mediterranean Basin. [PDF]
Salvo-Tierra ÁE +2 more
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The raising and westward expansion of central Tibet. [PDF]
Zhao C +15 more
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Soil erosion susceptibility assessment in the Bistrița River basin (Romania) using machine learning algorithms and GIS. [PDF]
Muratoreanu G +8 more
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New faunistic records of chironomids and phantom midges (Diptera, Chironomidae and Chaoboridae) from Ukraine indicate recent climatic refugia in the Eastern Carpathians. [PDF]
Bitušík P +3 more
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Detection of fractured zones, faults, and cavities by high resolution muon tomography in the Buda Hills. [PDF]
Balázs L +4 more
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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.
Dušan Majcin +6 more
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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.
Dušan Majcin +6 more
openaire +3 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.
Krzysztof Birkenmajer +3 more
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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.
Krzysztof Birkenmajer +3 more
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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 ...
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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 ...
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