Pregled bibliografske jedinice broj: 394969
Late Variscan (Latest Carboniferous - Early Permian) Late- and Post-orogenic Environments in the Circum Panonnian Region
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 (poster, nije recenziran, sažetak, ostalo)
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Naslov
Late Variscan (Latest Carboniferous - Early Permian) Late- and Post-orogenic Environments in the Circum Panonnian Region
Autori
Vozârovâ, A. ; Ebner, F. ; Kovâcs, S. ; Krâutner, H.G. ; Szederkenyi, T. ; Krstić, B. ; Sremac, J. ; Tomljenović, B. ; Novak, M.
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, ostalo
Izvornik
Proceedings - 18th Congress of the Carpathian - Balkan Geological Association
/ - Beograd : National Commutee of the Carpathian-Balkan Geological Association, Serbian Geological Society, 2006, 651-654
Skup
18th Congress of the Carpathian - Balkan Geological Association
Mjesto i datum
Beograd, Srbija, 03.09.2006. - 06.09.2006
Vrsta sudjelovanja
Poster
Vrsta recenzije
Nije recenziran
Ključne riječi
Late Carboniferous; Permian; Circum Pannonian Region; paleoenvironments; paleogeography; Variscan
Sažetak
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 lithosphè ; 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.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
0119404
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb,
Rudarsko-geološko-naftni fakultet, Zagreb
