Throughout the initial collision in the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (twelve mi) or more, remarkably metamorphosed, really deformed, and partly remelted through the Eocene Interval to sort gneiss. Later, the K2 Gneiss was then intruded by leucogranite dikes and finally https://cruzngxof.bloggerchest.com/32915121/detailed-notes-on-am-2201