| NEHYBA, Slavomír a Reinhard ROETZEL. Depositional environment and provenance analyses of the Zobing Formation (Upper Carboniferous-Lower Permian), Austria. Austrian Journal of Earth Sciences. Wien: Geological Society of Austria, 2015, roč. 108, č. 2, s. 245-276. ISSN 2072-7151. |
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@article{1336473,
author = {Nehyba, Slavomír and Roetzel, Reinhard},
article_location = {Wien},
article_number = {2},
keywords = {Zöbing Formation; Upper Carboniferous-Lower Permian; facies and provenance analyse; terrestrial deposits; terminal fluvial system},
language = {eng},
issn = {2072-7151},
journal = {Austrian Journal of Earth Sciences},
title = {Depositional environment and provenance analyses of the Zobing Formation (Upper Carboniferous-Lower Permian), Austria},
volume = {108},
year = {2015}
}
TY - JOUR
ID - 1336473
AU - Nehyba, Slavomír - Roetzel, Reinhard
PY - 2015
TI - Depositional environment and provenance analyses of the Zobing Formation (Upper Carboniferous-Lower Permian), Austria
JF - Austrian Journal of Earth Sciences
VL - 108
IS - 2
SP - 245-276
EP - 245-276
PB - Geological Society of Austria
SN - 20727151
KW - Zöbing Formation
KW - Upper Carboniferous-Lower Permian
KW - facies and provenance analyse
KW - terrestrial deposits
KW - terminal fluvial system
N2 - The deposits of the Upper Carboniferous to Lower Permian Zöbing Formation in Lower Austria have been studied by a widerange of sedimentological methods in several limited outcrops. Four facies associations were identified: (a) non-channelized finegrained deposits; (b) channelized sandstones, (c) non-channelized conglomerates, and (d) channelized conglomerates. Non-channelized fine-grained sediments are interpreted as deposits in shallow, semi-permanent pools on floodplains. Channelized sandstones are associated with fluvial processes and mostly represent crevasse channels cut into the floodplains. Channelized conglomerates originated from coarse-grained confined and hyperconcentrated flows. Non-channelized conglomerates are interpreted as sediments of alluvial fan and alluvial plain systems. A terminal fluvial system developed under a semi-arid to arid climatic regime is supposed to be the depositional environment of the Zöbing Formation.
ER -
NEHYBA, Slavomír a Reinhard ROETZEL. Depositional environment and provenance analyses of the Zobing Formation (Upper Carboniferous-Lower Permian), Austria. \textit{Austrian Journal of Earth Sciences}. Wien: Geological Society of Austria, 2015, roč.~108, č.~2, s.~245-276. ISSN~2072-7151.
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