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

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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