Over the initial collision of the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (twelve mi) or maybe more, extremely metamorphosed, highly deformed, and partly remelted throughout the Eocene Period to type gneiss. Later, the K2 Gneiss was then intruded by leucogranite dikes And https://rafaelgxpfv.bloggadores.com/32216848/chill-x-an-overview