 | Taalab, Sherif A., Abdel-Rahman, Ahmed M., El-Awny, Hamada, Awad, Hamdy A., Zakaly, Hesham M. H., Fahmy, Wael, Ene, Antoaneta (2023) Petrogenesis and Tectonic Evolution of Kab Amiri Ophiolites and Island-Arc Assemblages, Central Eastern Desert, Egypt: Petrological and Geochemical Constraints. Minerals, 13 (4) 528 doi:10.3390/min13040528 | Journal (article/letter/editorial) | | Evolution of Kab Amiri Ophiolites and Island-Arc Assemblages, Central Eastern Desert, Egypt: Petrological...Faculty of Science, Al-Azhar University, Cairo 11884, Egypt Geology Department, Faculty of Science, Al-Azhar...Al-Azhar University, Assiut Branch, Assiutt 71524, Egypt Institute of Physics and Technology, Ural Federal University...(A.E.) Abstract: The Kab Amiri area in the Central Eastern Desert (CED) of Egypt comprises ophiolitic...geodynamic evolution of the CED ophiolitic belt. The Kab Amiri ophiolite is dismembered, comprising serpentinites |  | Sherif, Mahmoud I., Ghoneim, Mohamed F., Heikal, Mohamed Th. S., El Dosuky, Bothina T. (2013) Perogenesis of granites, Sharm El-Sheikh area, South Sinai, Egypt: petrological constrains and tectonic evolution. Mineralogy and Petrology, 107 (5) 765-783 doi:10.1007/s00710-013-0267-5 | Journal (article/letter/editorial) | | of granites, Sharm El-Sheikh area, South Sinai, Egypt: petrological constrains and tectonic evolution...granites of the Sharm El-Sheikh area in south Sinai, Egypt belong to collisional and post-collisional Magmatism...Faculty of Science, Tanta University, Tanta 31527, Egypt e-mail: mahmoud.sherif@science.tanta.edu.eg Introduction...(in part), mostly hyphenate pinkish red to hyphenate whitish red and they are mainly syenogranites ranging...crystals up to 7 mm long. It is variably altered to saussurite shreds. Biotite is the common mafic mineral and |
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