Over the Preliminary collision of the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (twelve mi) or even more, really metamorphosed, really deformed, and partially remelted in the course of the Eocene Time period to form gneiss. Afterwards, the K2 Gneiss was then intruded https://louisskarh.csublogs.com/39785454/497-fundamentals-explained