Through the First collision on the Asia and Indian plates, this granitic batholith was buried to depths of about 20 kilometres (12 mi) or even more, highly metamorphosed, extremely deformed, and partially remelted during the Eocene Period to sort gneiss. Later, the K2 Gneiss was then intruded by leucogranite dikes And https://yucatan-fire23567.activosblog.com/32024679/k2-options