Chill X - An Overview
In the Preliminary collision in the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (12 mi) or more, extremely metamorphosed, hugely deformed, and partly remelted during the Eocene Interval to form gneiss. Later on, the K2 Gneiss was then intruded by leucogranite dikes And eventually exhumed and upli