Results 161 to 170 of about 1,927,585 (215)
Foraminifera from the Eocene Variegated Shales near Barwinek (Magura Unit, Outer Carpathians), the type locality of Noth (1912) revisited [PDF]
, 2005 Cieszkowski, M, Kaminski, MA, Kender, S
core
Granites and granite caves in the Western Carpathians
, 2008 Gaál, l., Bella, P.
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Integrated modelling and rheological study of the western Carpathians.
Geologica Carpathica, 1999 Bielik, M., Zeyen, H., Lankreijer, A.C.
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Amphibian breeding site characteristics in the Western Carpathians, Poland
, 2001 Babik, Wiesław, Rafiński, Jan
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Special Publications, 2021
Micritic sediments containing dark, discrete, organic-rich burrows, situated in a light grey background carbonate mud, were deposited over a broad geographical area in deep-shelf, bathyal and basinal environments in the western margin of the Tethys Ocean
V. Šimo, M. Reolid
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Micritic sediments containing dark, discrete, organic-rich burrows, situated in a light grey background carbonate mud, were deposited over a broad geographical area in deep-shelf, bathyal and basinal environments in the western margin of the Tethys Ocean
V. Šimo, M. Reolid
semanticscholar +1 more source
Permian lamprophyres from the Western Carpathians: a review
Geological Society, London, Special Publications, 2021Abstract Calc-alkaline lamprophyres from the Western Carpathians occur as dykes and sills in the crystalline complexes (predominantly granites and gneisses) of the Tatric Unit. Some of the lamprophyre dykes have been strongly overprinted by tectonism and hydrothermal fluid ingress.
Ján Spišiak +6 more
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Neogene exhumation in the Outer Western Carpathians
Terra Nova, 2011Terra Nova, 23, 283–291, 2011AbstractApatite fission‐track analysis was used to investigate the Cenozoic tectonic evolution of the Polish sector of the Outer Western Carpathians, where thrusting was overlapped by extension in the last 10 Ma. The results show a general decrease of burial degree towards the European foreland and a range of cooling ages ...
ZATTIN, MASSIMILIANO +4 more
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Sedimentology, 2020
The anisotropy of magnetic susceptibility is a well‐known geological proxy in revealing the directional tectonic and sedimentological features of rocks, although it can be ambiguous in situations where these two factors co‐occur.
A. Stachowska +5 more
semanticscholar +1 more source
The anisotropy of magnetic susceptibility is a well‐known geological proxy in revealing the directional tectonic and sedimentological features of rocks, although it can be ambiguous in situations where these two factors co‐occur.
A. Stachowska +5 more
semanticscholar +1 more source
Tectonics, 1995
On the basis of field studies and subsurface data, this first balanced transect crosses most of the Carpathian foreland basin and the entire Polish Western Carpathian thrust units (Outer flysch nappes, Pieniny Klippen Belt, and Inner Carpathian Tatric thrust sheets).
E. Roca +4 more
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On the basis of field studies and subsurface data, this first balanced transect crosses most of the Carpathian foreland basin and the entire Polish Western Carpathian thrust units (Outer flysch nappes, Pieniny Klippen Belt, and Inner Carpathian Tatric thrust sheets).
E. Roca +4 more
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Magnetotelluric Investigation in the Polish Western Carpathians
60th EAGE Conference and Exhibition, 1998Objectives of the magnetotelluric survey in the Carpathians (southern Poland) include identification of the structure of the Carpathian orogen and the topography of the crystalline basement as well as prospecting for hydrocarbons.
J. Miecznik +3 more
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