Fascination About 5F-PB-22
Over the initial collision in the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (twelve mi) or even more, remarkably metamorphosed, highly deformed, and partially remelted in the course of the Eocene Period to variety gneiss. Afterwards, the K2 Gneiss was then intruded by leucogranite dikes And at