Brunovistulian terrane (Bohemian Massif, Central Europe) from late Proterozoic to late Paleozoic: a review

Warning

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

Authors	KALVODA JIŘÍ BÁBEK Ondřej FATKA Oldřich LEICHMANN Jaromír MELICHAR Rostislav NEHYBA Slavomír ŠPAČEK Petr
Year of publication	2008
Type	Article in Periodical
Magazine / Source	International Journal of Earth Sciences
MU Faculty or unit	Faculty of Science
Citation
Web	http://www.springerlink.com/content/g8w105g575326m64/fulltext.pdf
Field	Geology and mineralogy
Keywords	Bohemian Massif Brunovistulian terrane Paleogeography Tectonic structure Variscan orogeny
Description	The Brunovistulian terrane represents a microcontinent of enigmatic Proterozoic provenance that was located at the southern margin of Baltica in the early Paleozoic.
Related projects:	Interactions among the chemicals, environment and biological systems and their consequences on the global, regional and local scales (INCHEMBIOL)