Horní Bory. Structural and metamorphic evolution of the high-T/high-P Gföhl unit (Moldanubicum).

Warning

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

Authors	KOTKOVÁ Jana MELICHAR Rostislav
Year of publication	2003
Type	Article in Proceedings
Conference	Geology without frontiers: magmatic and metamorphic evolution of Central European Variscides. Excursion Guide.
MU Faculty or unit	Faculty of Science
Citation
Field	Geology and mineralogy
Keywords	granulite; Horní Bory quarry; granite; metamorphic evolution; geochemistry; structural context; Bohemian Massif
Description	The paper gives details on the petrology, geochemistry, structual and metamorphic evolution of granulites in the Bory granulite massif. It also contains a structural sketch of the quarry and brings information on products of partial melting and on granitoid rocks intruding along the subvertical shear zones.
Related projects:	Partial melting of rocks in the root zone of the Variscan orogenic belt (Moldanubian Zone, Bohemian Massif) Geological Processes and their Environmental Impact - Contact of the Variscides and Alpides