The Mount El-Sibai pluton intruded into metasedimentary, metavolcanic, and Pan-African calc-alkaline granitic host rocks. The contacts of this elliptical body are parallel to the Red Sea axis. Mineralogically, the Mount El-Sibai granites are hypersolvus,
Description:
Thesis (M.S.)--American University of Beirut. Department of Geology, 1999;"Advisor: Dr. Abdel-Fattah M. Abdel-Rahman, Associate Professor, Geology--Member of Committee: Dr. Sara Spencer, Assistant Professor, Geology--Member of Committee: Dr. Ulrich Kortz,
