CONSIDERATIONS TO KNOW ABOUT JWH-122

Over the Original collision from the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (twelve mi) or more, very metamorphosed, extremely deformed, and partially remelted during the Eocene Period to variety gneiss. Later on, the K2 Gneiss was then intruded by leucogranite dikes and finally exhumed and