Results 181 to 190 of about 19,454 (237)

Integrated modelling and rheological study of the western Carpathians.

open access: yesGeologica Carpathica, 1999
Bielik, M., Zeyen, H., Lankreijer, A.C.
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Permian lamprophyres from the Western Carpathians: a review

Geological Society, London, Special Publications, 2021
Abstract 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, 2011
Terra 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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Pre‐Neogene evolution of the Western Carpathians: Constraints from the Bochnia‐Tatra Mountains section (Polish Western Carpathians)

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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Magnetotelluric Investigation in the Polish Western Carpathians

60th EAGE Conference and Exhibition, 1998
Objectives 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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Seismicity of the Western-Carpathians

Acta Geodaetica et Geophysica Hungarica, 2005
The source parameters and dimensions of the three most important earthquakes (Zsolna - Jan. 15, 1858, Io = VIII EMS; Joko - Jan. 9, 1906, Io = VIII EMS; Joko- Jan. 16, 1906, Io = VII-VIII EMS) of the area studied are estimated as follows: Event (Magnitude, Rupture area, Max. Displacement); Jan. 15, 1858 Zsolna (5.5 Ms, 22-36 km2, 8-11 cm); Jan. 9, 1906
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