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

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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)