Provenance of the Lower Carboniferous Culm sediments of the Drahany Upland (Czech Republic), derived from garnet chemistry

Warning

This publication doesn't include Faculty of Education. It includes Faculty of Science. Official publication website can be found on muni.cz.

Authors	ČOPJAKOVÁ Renata SULOVSKÝ Petr OTAVA Jiří
Year of publication	2001
Type	Article in Periodical
Magazine / Source	Mitteilungen der Österr. Mineral. Gesellschaft
MU Faculty or unit	Faculty of Science
Citation
Field	Geology and mineralogy
Keywords	garnet chemistry; sediment provenance; Culm; Drahany Upland
Description	The provenance of Culm sediments was deciphered using the specific features of detrital garnet chemistry. The study revealed a sudden change in source area within the Myslejovice Formation.
Related projects:	Exhumation of the Variscan lower crust - constraints Viséan siliciclastics (Eastern Bohemian Massif)