Throughout the initial collision from the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (twelve mi) or even more, extremely metamorphosed, highly deformed, and partly remelted in the Eocene Period of time to kind gneiss. Later, the K2 Gneiss was then intruded by leucogranite https://simonmohxv.develop-blog.com/39789039/a-simple-key-for-497-unveiled