CHILL X - AN OVERVIEW

In the course of the Preliminary collision on the Asia and Indian plates, this granitic batholith was buried to depths of about 20 kilometres (twelve mi) or maybe more, hugely metamorphosed, very deformed, and partly remelted in the course of the Eocene Time period to variety gneiss. Later on, the K2 Gneiss was then intruded by leucogranite dikes