In the course of the initial collision of the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (12 mi) or more, hugely metamorphosed, remarkably deformed, and partially remelted during the Eocene Period of time to type gneiss. Afterwards, the K2 Gneiss was then intruded https://sethnfxod.blogsumer.com/32230216/chill-x-an-overview