Through the First collision of your Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (12 mi) or more, remarkably metamorphosed, really deformed, and partially remelted over the Eocene Interval to form gneiss. Later, the K2 Gneiss was then intruded by leucogranite dikes And eventually https://jwh-01880234.activoblog.com/35207786/5-simple-techniques-for-xlr-11