In the course of the Original collision of the Asia and Indian plates, this granitic batholith was buried to depths of about 20 kilometres (12 mi) or more, remarkably metamorphosed, really deformed, and partly remelted throughout the Eocene Time period to kind gneiss. Later on, the K2 Gneiss was then intruded https://gunnerbujnu.buyoutblog.com/32993046/top-guidelines-of-am678