Abstract
P-T conditions of sapphirine bearing granulites from a new locality from the north eastern part of Gujarat range from 8.2–8.8 kbars at T of 950°C. The discovery of this UHT assemblage in the north western part of the Indian shield bordering the Aravalli-Delhi fold belt provides additional evidences for India-Madagascar connection, linking the Aravalli- Malani sequences to similar lithologies in northern Madagascar.
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