Detailed Information on Publication Record
2001
Depositional environment of the "Old Red" sediments in the Brno area (South-eastern part of the Rhenohercynian zone, Bohemian Massif)
NEHYBA, Slavomír, Jaromír LEICHMANN and Jiří KALVODABasic information
Original name
Depositional environment of the "Old Red" sediments in the Brno area (South-eastern part of the Rhenohercynian zone, Bohemian Massif)
Authors
Edition
Geologica Carpathica, Bratislava, SAV, 2001, 1335-0552
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10500 1.5. Earth and related environmental sciences
Country of publisher
Slovakia
Confidentiality degree
není předmětem státního či obchodního tajemství
Impact factor
Impact factor: 0.167
RIV identification code
RIV/00216224:14310/01:00004419
Organization unit
Faculty of Science
UT WoS
000171603200001
Keywords in English
Early Paleozoic; monomict-quartzose clastics; conglomerates; sheetfloods
Změněno: 26/9/2001 10:14, prof. RNDr. Slavomír Nehyba, Dr.
Abstract
V originále
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).
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