2002•Unpublished venueRequires access
Sedimentary Petrography and Provenance Study as an Indicator ofthe Evolution of Sedimentary Basin - southern part of theBoskovice Furrow (Czech Rep.)
Filip Jelínek, Slavomı́r Nehyba, Jaromı́r Leichmann
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Abstract
Provenance study of the clastic deposits of the asymmetric half
graben basin can bring important data of the tectonic evolution
of the oposite margins. Tectonic processes influenced the basin
morphology, the gradient of the basin bottom. distribution of
depositional environments and cyclicity of deposits. Different
role of the axial and transverse transport within the basin can
be assumed.