Throughout the First collision from the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (twelve mi) or maybe more, really metamorphosed, extremely deformed, and partially remelted through the Eocene Period of time to form gneiss. Later, the K2 Gneiss was then intruded by leucogranite https://yucatan-fire58147.thezenweb.com/the-smart-trick-of-algerian-blend-that-nobody-is-discussing-70946459