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Conditions of the depositions of the paleogene formation in the Racza zone to the south of Żywiec (Magura nappe, Polish outer Carpathians) [PDF]
, 2009 Wójcik, Ewa
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Cenozoic freshwater carbonates of the Central Carpathians (Slovakia) : facies, environments, hydrological control and depositional history [PDF]
, 2015 Bella, Pavel +2 more
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Poręba Wielka : small-scale faulting in the Rača and Bystrica slices of the Magura Nappe
, 2001 openaire +1 more source
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Deformation bands and the history of folding in the Magura nappe, Western Outer Carpathians (Poland)
Tectonophysics, 1998Abstract 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, Antoni K Tokarski
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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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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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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
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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
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Proceedings, 2013
The aim of the present studies was to evaluate thermal maturity of internal nappes in the Polish segment of the Outer Carpathians using independent methodologies. Studies were performed on twenty one claystone samples collected from natural exposures The age of sampled rocks ranges from Late Cretaceous to Oligocene.
M.W. Waliczek, A.Ś. Świerczewska
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The aim of the present studies was to evaluate thermal maturity of internal nappes in the Polish segment of the Outer Carpathians using independent methodologies. Studies were performed on twenty one claystone samples collected from natural exposures The age of sampled rocks ranges from Late Cretaceous to Oligocene.
M.W. Waliczek, A.Ś. Świerczewska
openaire +1 more source