Through the Original collision of the Asia and Indian plates, this granitic batholith was buried to depths of about 20 kilometres (twelve mi) or even more, remarkably metamorphosed, really deformed, and partly remelted in the Eocene Time period to form gneiss. Later on, the K2 Gneiss was then intruded by leucogranite https://jwh-07393604.bloggazza.com/32036885/the-smart-trick-of-jwh-073-that-nobody-is-discussing