Contrasting Metamorphic Evolution of HP Rocks in the Gföhl Unit of the Kutná Hora Crystalline Complex and the Moldanubian Zone in Austria

Geolines | January 1, 2006| | Copyright

The uppermost part (Bestvina and Malín formations) of the Kutná Hora Crystalline Complex is due to presence of HP/HT granulites, garnet peridotites and eclogites are generally correlated with the Gföhl complex in the Moldanubian zone. We have studied felsic granulites, kyanite-bearing migmatites and migmatitic gneisses of the Gföhl-relted unit in the Kutná Hora Crystalline Complex and in the Moldanubian zone of Waldviertel in Austria. In order to analyse PT evolution of individual lithologies we have constructed pseudosections in the NCKF-MASH system using the THERMOCALC software (Powell ...

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