In the initial collision in the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (twelve mi) or maybe more, extremely metamorphosed, very deformed, and partly remelted during the Eocene Time period to sort gneiss. Afterwards, the K2 Gneiss was then intruded by leucogranite dikes https://cp-4790901.is-blog.com/39418511/5-simple-techniques-for-xlr-11