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Late Variscan (Latest Carboniferous - Early Permian) Late- and Post-orogenic Environments in the Circum Panonnian Region (CROSBI ID 548056)

Prilog sa skupa u zborniku | sažetak izlaganja sa skupa

Vozârovâ, A. ; Ebner, F. ; Kovâcs, S. ; Krâutner, H.G. ; Szederkenyi, T. ; Krstić, B. ; Sremac, J. ; Tomljenović, B. ; Novak, M. Late Variscan (Latest Carboniferous - Early Permian) Late- and Post-orogenic Environments in the Circum Panonnian Region // Proceedings - 18th Congress of the Carpathian - Balkan Geological Association. Beograd: National Commutee of the Carpathian-Balkan Geological Association, Serbian Geological Society, 2006. str. 651-654

Podaci o odgovornosti

Vozârovâ, A. ; Ebner, F. ; Kovâcs, S. ; Krâutner, H.G. ; Szederkenyi, T. ; Krstić, B. ; Sremac, J. ; Tomljenović, B. ; Novak, M.

engleski

Late Variscan (Latest Carboniferous - Early Permian) Late- and Post-orogenic Environments in the Circum Panonnian Region

The explanation to the map of tectonostratigraphic terranes and the Latest Carboniferous-Early Permian late-orogenic paleoenvironments of the Circum Pannonian Region (CPR) also includes the Upper Bashkirian-Moscovian marine early molasse stage as well as the Upper Permian post-orogenic stage, with gradual connection to the beginning of the Alpine orogenic cycle. Shallow marine siliciclastic or carbonate siliciclastic overstep sequences started in the internal part of the Variscan orogenic belt during the Serpukhovian and Uppermost Bashkirian-Moscovian. They unconformably overlapped the variably metamorphosed Variscan basement or weakly deformed and metamorphosed syn-orogenic Lower to Middle Carboniferous flysch sediments. Post-Variscan rifting largely affected the Variscan orogenic belt by reactivation of the weak Variscan lithosph&egrave ; re. Terrestrial overstep sequences started within internal part of the Variscan orogenic belt during the Latest Carboniferous with graduate continuation to terrestrial-shallow water carbonate-siliciclastic sequences in its external part through the Permian. The Alpine northward shifting transgression started during the Middle/Upper Permian in the south and during the Lower Triassic in the north.

Late Carboniferous; Permian; Circum Pannonian Region; paleoenvironments; paleogeography; Variscan

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Podaci o prilogu

651-654.

2006.

objavljeno

Podaci o matičnoj publikaciji

Proceedings - 18th Congress of the Carpathian - Balkan Geological Association

Beograd: National Commutee of the Carpathian-Balkan Geological Association, Serbian Geological Society

Podaci o skupu

18th Congress of the Carpathian - Balkan Geological Association

poster

03.09.2006-06.09.2006

Beograd, Srbija

Povezanost rada

Geologija