During the initial collision in the Asia and Indian plates, this granitic batholith was buried to depths of about 20 kilometres (twelve mi) or even more, highly metamorphosed, highly deformed, and partially remelted in the course of the Eocene Period of time to type gneiss. Later on, the K2 Gneiss was https://claytonuqiuf.blogunteer.com/32008128/a-simple-key-for-jwh-201-unveiled