Abstract
Um Taghir area located in theCentral Eastern Desert of Egypt a long road of Safaga-Qena. Itis represented by island arc related rocks that are intruded by late to post tectonic magmatism. The island arc belonging to oceanic terrain, divided into metavolcaniclastic and metagabrroic rocks. Metavolcanoclastic sequence is represented as the older rock unit of the study area,it is noted that metavolcanoclastic intruded by metagabbro. Island arc assemblage is classified into schist and metagabbro that give clean different of their mineralconstituents according to petrographical studies. Geochemically , the investigated rock units and most of dikes have sub alkaline nature. Tectonically , metavolcanoclastic sequence is related to back arc basin basalts, while metagabbro related to volcanic arc.
Sign-in/Register to access full text options 
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
