West Gabal Monqul, Eastran Desert, Egypt - Kharbish, Sherif;Azzaz, Said;El-Alfy, Hesham
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West of Gabal Monqul represents a part of the north Eastern Desert of Egypt, covering ~ 470km2. The area are composed of Island arc system, Calc-alkaline plutonites and Rifting system. The interpretations of geochemistry and mineral chemistry verified the calc-alkaline arc suite for the investigated metavolcanics and metagabbro-diorite association. Older granitoids are most probably derived from unfractionated, calc-alkaline metaluminous magma which are tectonically emplaced in arcorogenic suite.

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Produktbeschreibung
West of Gabal Monqul represents a part of the north Eastern Desert of Egypt, covering ~ 470km2. The area are composed of Island arc system, Calc-alkaline plutonites and Rifting system. The interpretations of geochemistry and mineral chemistry verified the calc-alkaline arc suite for the investigated metavolcanics and metagabbro-diorite association. Older granitoids are most probably derived from unfractionated, calc-alkaline metaluminous magma which are tectonically emplaced in arcorogenic suite.
Autorenporträt
Prof. Sherif Kharbish (Ph.D.) is a mineralogist. He graduated the Vienna University as a student of academician Ao. Prof. Dr. Anton Beran. He studied the Raman spectra of sulfosalts and sulfides. He is a professor at the Suez University (Egypt).He wrote 70 articles, scientific publications and books.