Through the Original collision of the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (12 mi) or more, hugely metamorphosed, remarkably deformed, and partially remelted during the Eocene Period to sort gneiss. Later on, the K2 Gneiss was then intruded by leucogranite dikes and https://smoke18383.actoblog.com/33615520/top-latest-five-am-scs-urban-news