In the initial collision on the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (twelve mi) or maybe more, highly metamorphosed, highly deformed, and partially remelted through the Eocene Period of time to variety gneiss. Afterwards, the K2 Gneiss was then intruded by leucogranite https://spicesilver38371.losblogos.com/32143881/details-fiction-and-am-2201