Results 81 to 90 of about 19,531 (99)
Central European Variscan Basement in the Outer Carpathians: A Case Study From the Magura Nappe, Outer Western Carpathians, Poland [PDF]
Minerals (Basel, Switzerland), 2021 Exotic crystalline blocks within the Outer Carpathian flysch have the potential to establish the nature of their eroded basement source(s) and thus to reconstruct the paleogeography of the Outer Carpathians. Petrological investigations (including mineral analyses) coupled with zircon and apatite U-Pb dating were performed on an exotic crystalline block
Aleksandra Gawęda +2 more
exaly +6 more sources
Geology of the Magura Nappe in the Osielec Area With Emphasis on an Eocene Olistostrome With Metabasite Olistoliths (Outer Carpathians, Poland) [PDF]
Annales Societatis Geologorum Poloniae, 2017 The Magura Nappe in the Polish sector of the Outer Carpathians consists of four tectonic subunits characterized by differing development of facies. From the south to the north, they include the Siary, Raca, Bystrica and Krynica subunits. The sedimentary succession in the Raca Subunit in the vicinity of the village of Osielec is composed of Campanian ...
Mateusz Szczech +2 more
exaly +6 more sources
Acta Geologica Hungarica, 2005 The Magura Nappe is the innermost tectonic unit of the Western Flysch Carpathians and is linked with the Rheno-Danubian flysch of the Eastern Alps. Toward the east this unit runs as an arc from Austria through the Czech Republic, Slovakia and Poland, and then narrows in Eastern Slovakia before disappearing east of Uzhhorod (Trans-Carpathian Ukraine ...
Marta Oszczypko-Clowes +2 more
exaly +4 more sources
Petrogenesis of Metabasite Olistoliths From the Magura Nappe in the Polish Western Outer Carpathians
Geological QuarterlyMaciej Kania +2 more
exaly +3 more sources
Some of the next articles are maybe not open access.
Related searches:
Related searches:
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 Teresa Świerczewska
exaly +2 more sources
History of Folding in the Magura Nappe, Outer Carpathians, Poland
2018A.K. Tokarski, A. Świerczewska
exaly +2 more sources
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
openaire +1 more source
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
openaire +1 more source
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
openaire +1 more source
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