Over the initial collision of your Asia and Indian plates, this granitic batholith was buried to depths of about 20 kilometres (twelve mi) or maybe more, extremely metamorphosed, hugely deformed, and partly remelted during the Eocene Period to type gneiss. Afterwards, the K2 Gneiss was then intruded by leucogranite dikes And https://ricardokbjvf.howeweb.com/33585135/not-known-details-about-5f-ab-pinaca