Through the initial collision with the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (twelve mi) or even more, very metamorphosed, really deformed, and partially remelted during the Eocene Period to form gneiss. Later, the K2 Gneiss was then intruded by leucogranite dikes and https://conneriszfj.blogocial.com/an-unbiased-view-of-ab-chiminaca-68757776