Results 81 to 90 of about 17,227 (96)

History of jointing in the medial segment of the Magura Nappe

, 2001
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Poręba Wielka : small-scale faulting in the Rača and Bystrica slices of the Magura Nappe

, 2001
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The nannofossil biostratigraphy of the youngest deposits of the Magura Nappe (East of the Skawa river, Polish Flysch Carpathians)

, 2001
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Jointing in Eocene fysch strata ofthe mid-eastern Magura Nappe, Polish outer Carpathians : implications for the timing of deformation

, 2000
Oszczypko, Nestor, Zuchiewicz, Witold
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Deformation bands and the history of folding in the Magura nappe, Western Outer Carpathians (Poland)

Tectonophysics, 1998
Abstract Deformation bands ( db ) which are indicative for soft-sediment deformation during the folding of flysch sediments are widespread within the Eocene strata of the Magura nappe. Four types of db have been distinguished: (1) db with no cataclasis of detrital sand grains; (2) db with traces of feldspar cataclasis; (3) db with strong ...
Anna Świerczewska
exaly   +2 more sources

Paleocurrent analysis and paleogeography of the Biele Karpaty Unit (Magura Nappe, Outer Western Carpathians)

International Journal of Earth Sciences, 2022
František Teťák
exaly   +2 more sources

Deep Water Agglutinated Foraminiferal Assemblages from Upper Cretaceous Red Shales of the Magura Nappe / Polish Outer Carpathians

1990
At the Cenomanian/Turonian boundary in the Outer Carpathian basin the sedimentation of black and green Radiolarian shales was replaced by deposition of variegated shales reflecting a distinct change in sedimentary conditions from anaerobic to aeorobic. Sedimentation of the Turonian to Lower Senonian variegated shales preceded uplift of the intrabasinal
Ewa Malata, Nestor Oszczypko
exaly   +2 more sources

History of folding in the Magura nappe, Outer Carpathians, Poland

2018
A.K. Tokarski, A. Świerczewska
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Diverse tiering patterns in Paleogene flysch trace fossils, Magura nappe, Carpathian Mountains, Poland

Ichnos, 1991
Alfred Uchman
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Sediment dispersal and provenance in the Silesian, Dukla and Magura flysch nappes (Outer Carpathians, Poland)

Geologische Rundschau, 1992
The Polish Outer Carpathians consist of several flysch series of unknown original basement. They were deposited from Late Jurassic to Miocene in a large basin dissected by tectonically uplifted ridges (cordillieras) which acted as source terrains. The actual nappe pile is correlated with palaeogeographic basin realms.
Winkler, Wilfried, Slaczka, Andrzej
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