In the Preliminary collision of your Asia and Indian plates, this granitic batholith was buried to depths of about 20 kilometres (12 mi) or more, highly metamorphosed, extremely deformed, and partially remelted over the Eocene Period to form gneiss. Later on, the K2 Gneiss was then intruded by leucogranite dikes and https://knoxlankz.therainblog.com/31940492/5-simple-techniques-for-xlr-11