Throughout the Original collision on the Asia and Indian plates, this granitic batholith was buried to depths of about 20 kilometres (12 mi) or even more, hugely metamorphosed, very deformed, and partially remelted in the Eocene Period of time to type gneiss. Afterwards, the K2 Gneiss was then intruded by leucogranite https://jwh-01812109.blog-gold.com/41383974/the-greatest-guide-to-algerian-blend