Over the initial collision in the Asia and Indian plates, this granitic batholith was buried to depths of about 20 kilometres (twelve mi) or maybe more, highly metamorphosed, very deformed, and partially remelted in the course of the Eocene Period of time to variety gneiss. Afterwards, the K2 Gneiss was then https://am67820395.blog-eye.com/33085045/5-tips-about-jwh-250-you-can-use-today