Dolnokarboński flisz (kulm) w rejonie Głubczyc
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Abstract:
Lower Carboniferous Flysch in the Glubczyce region (Lower Silesia)
The following lithostratigraphic units are established in the Lower Carboniferous flysch sequence cropping out in the region of Glubczyce: the lower unit — the Horni Benesov Formation consisting of greywackes and conglomerates alternating with shales; the middle unit — the Moravice Formation consisting of shales and slates, with two coarse-grained members: the Ciermiecice sandstone member and the Pielgrzymow conglomerate member; the upper unit — the Hradek Formation consisting of greywackes and shales. Formal definitions of these lithostratigraphic units are given. The tectonic structure of the Lower Carboniferous flysch rocks in the Glubczyce region is described.Keywords:
Flysch
SLATES
Conglomerate
Westphalian sovereignty
Stratigraphic unit
Sequence (biology)
Phyllite
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