In the First collision of the Asia and Indian plates, this granitic batholith was buried to depths of about 20 kilometres (12 mi) or even more, remarkably metamorphosed, really deformed, and partly remelted in the course of the Eocene Period of time to kind gneiss. Afterwards, the K2 Gneiss was then https://spice-silver02456.loginblogin.com/40130536/indicators-on-5f-pb-22-you-should-know