During the Preliminary collision of the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (12 mi) or maybe more, remarkably metamorphosed, extremely deformed, and partially remelted during the Eocene Time period to kind gneiss. Afterwards, the K2 Gneiss was then intruded by leucogranite dikes https://yucatan-fire60471.kylieblog.com/33494676/detailed-notes-on-am-2201