| NEHYBA, Slavomír, Jaromír LEICHMANN a Jiří KALVODA. Depositional environment of the "Old Red" sediments in the Brno area (South-eastern part of the Rhenohercynian zone, Bohemian Massif). Geologica Carpathica. Bratislava: SAV, 2001, roč. 52, č. 4, s. 195-203. ISSN 1335-0552. |
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@article{368613,
author = {Nehyba, Slavomír and Leichmann, Jaromír and Kalvoda, Jiří},
article_location = {Bratislava},
article_number = {4},
keywords = {Early Paleozoic; monomict-quartzose clastics; conglomerates; sheetfloods},
language = {eng},
issn = {1335-0552},
journal = {Geologica Carpathica},
title = {Depositional environment of the "Old Red" sediments in the Brno area (South-eastern part of the Rhenohercynian zone, Bohemian Massif)},
volume = {52},
year = {2001}
}
TY - JOUR
ID - 368613
AU - Nehyba, Slavomír - Leichmann, Jaromír - Kalvoda, Jiří
PY - 2001
TI - Depositional environment of the "Old Red" sediments in the Brno area (South-eastern part of the Rhenohercynian zone, Bohemian Massif)
JF - Geologica Carpathica
VL - 52
IS - 4
SP - 195
EP - 195
PB - SAV
SN - 13350552
KW - Early Paleozoic
KW - monomict-quartzose clastics
KW - conglomerates
KW - sheetfloods
N2 - Lower Devonian monomict-quartzose coarse-grained clastics are interpreted as the deposits of an alluvial fan built up mainly by catastrophic sheetfloods. The main sources were probably granites and gneisses, other components were derived from rhyolites, older siliciclastics sediments and low-grade metamorphic rocks. Rapid uplift, erosion dominated by mechanical weathering and multiple redeposition are supposed within the drainage basin. The flat alluvial fan was only slightly reworked and eroded during subsequent non-catastrophic overland flows (sedondary processes).
ER -
NEHYBA, Slavomír, Jaromír LEICHMANN a Jiří KALVODA. Depositional environment of the ''Old Red'' sediments in the Brno area (South-eastern part of the Rhenohercynian zone, Bohemian Massif). \textit{Geologica Carpathica}. Bratislava: SAV, 2001, roč.~52, č.~4, s.~195-203. ISSN~1335-0552.
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