Through the Preliminary collision of your Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (12 mi) or more, very metamorphosed, remarkably deformed, and partly remelted during the Eocene Period of time to variety gneiss. Afterwards, the K2 Gneiss was then intruded by leucogranite dikes https://connerrcrxt.blog-a-story.com/13551074/the-fact-about-ab-pinaca-that-no-one-is-suggesting