Publication details

P-T evolution of diamond-bearing intermediate granulites from North Bohemia: first results



Year of publication 2014
Type Conference abstract
MU Faculty or unit

Faculty of Science

Description Diamond and coesite inclusions discovered within garnet and kyanite in felsic and intermediate granulites of the Eger Crystalline Complex document ultrahigh- pressure conditions experienced by the rocks (Kotková et al. 2011). Such conditions significantly exceed previously determined peak metamorphic conditions (Kotková 1993) and they rather correspond to eclogite facies. However, these rocks later equilibrated under granulite facies. We investigated intermediate granulites from outcrops in Stráž nad Ohří in order to constrain their P-T evolution.

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