THE GREATEST GUIDE TO ALGERIAN BLEND

During the initial collision with the Asia and Indian plates, this granitic batholith was buried to depths of about 20 kilometres (12 mi) or more, highly metamorphosed, extremely deformed, and partially remelted through the Eocene Period to sort gneiss. Afterwards, the K2 Gneiss was then intruded by leucogranite dikes And eventually exhumed and up

Throughout the initial collision in the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (twelve mi) or even more, remarkably metamorphosed, really deformed, and partially remelted in the course of the Eocene Time period to kind gneiss. Later, the K2 Gneiss was then intruded by leucogranite dikes and