The Spačice eclogite : constraints on the P-T-t history of the Gfohl granulite terrane, Moldanubian zone, Bohemian massif.

Abstract

The eclogite assemblage (grnt+omph+qz) yields peak metamorphic condition of 18-20kbar and 900 - 1000 oC. The brief duration of HP/HT metamorphism, rapid cooling and exhumation of the Gfohl terrane consequence of litospheric delamination during E.Carbon.

Keywords

• P-T-t history
• eclogite
• moldanubian
• gfohl terrane
• Bohemian massif