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@article{699869,
author = {Otava, Jiří and Havíř, Josef},
article_location = {Warszawa},
article_number = {3},
keywords = {Culm facies; Variscan folding; slumping; stratigraphical polarity},
language = {eng},
issn = {1641-7291},
journal = {Geological Quarterly},
title = {Apparent contradiction between tectonics and deposition in overturned strata - a case study from the "Moravian Culm" (Czech Republic)},
volume = {50},
year = {2006}
}
TY - JOUR
ID - 699869
AU - Otava, Jiří - Havíř, Josef
PY - 2006
TI - Apparent contradiction between tectonics and deposition in overturned strata - a case study from the "Moravian Culm" (Czech Republic)
JF - Geological Quarterly
VL - 50
IS - 3
SP - 391-394
EP - 391-394
SN - 16417291
KW - Culm facies
KW - Variscan folding
KW - slumping
KW - stratigraphical polarity
N2 - An apparent contradiction between structural and sedimentological indications commonly used for discrimination of the overturned and non-overturned beds during geological mapping was found at Paršovice, a site situated in the easternmost part of the European Variscides. This outcrop of folded Lower Carboniferous siliciclastic rocks of the "Culm facies" lies on the NE margin of the Bohemian Massif, in the SE part of the Maleník Block (Moravia, Czech Republic). At the same site, a slump-related isoclinal fold was found. The apparent contradiction between structural (relation of cleavage and bedding) and sedimentological (flute casts on bed soles) indications is explained by a combination of successive phases of slump- and tectonically-related folding.
ER -
OTAVA, Jiří a Josef HAVÍŘ. Apparent contradiction between tectonics and deposition in overturned strata - a case study from the ''Moravian Culm'' (Czech Republic). \textit{Geological Quarterly}. Warszawa, 2006, roč.~50, č.~3, s.~391-394. ISSN~1641-7291.
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