During the Preliminary collision of your Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (twelve mi) or more, remarkably metamorphosed, really deformed, and partially remelted in the Eocene Period of time to variety gneiss. Later on, the K2 Gneiss was then intruded by leucogranite https://algerianblend52304.blog-ezine.com/33082514/not-known-details-about-5f-ab-pinaca