Throughout the Original collision from the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (12 mi) or maybe more, really metamorphosed, very deformed, and partly remelted over the Eocene Period of time to sort gneiss. Afterwards, the K2 Gneiss was then intruded by leucogranite https://yucatanfire03467.blogdanica.com/32948924/the-am-2201-diaries