AN UNBIASED VIEW OF AB-CHIMINACA

Over the Preliminary collision of the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (twelve mi) or more, hugely metamorphosed, highly deformed, and partly remelted during the Eocene Time period to form gneiss. Later on, the K2 Gneiss was then intruded by leucogranite dikes and finally exhumed and u