In the course of the Original collision in the Asia and Indian plates, this granitic batholith was buried to depths of about 20 kilometres (12 mi) or maybe more, hugely metamorphosed, really deformed, and partially remelted through the Eocene Interval to kind gneiss. Later, the K2 Gneiss was then intruded by https://andresokfyp.life3dblog.com/31977856/k2-options