E
E.S. Farahat
Researcher at Minia University
Publications - 24
Citations - 842
E.S. Farahat is an academic researcher from Minia University. The author has contributed to research in topics: Mafic & Partial melting. The author has an hindex of 14, co-authored 23 publications receiving 697 citations.
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Origin of I- and A-type granitoids from the Eastern Desert of Egypt: Implications for crustal growth in the northern Arabian Nubian Shield
TL;DR: In this article, Petrological and geochemical data are presented for a selection of the two groups, the I-type, El Bula tonalite-granodiorite suite, and the A-type Lomân alkali granites, with the aim of discussing their origin and geotectonic implications.
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Continental back-arc basin origin of some ophiolites from the Eastern Desert of Egypt
TL;DR: In this paper, geochemical and petrographical data of three ophiolitic pillow metavolcanic occurrences from the central Eastern Desert of Egypt are presented The investigated rocks show a subalkaline, tholeiitic affinity.
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Chrome-spinels in serpentinites and talc carbonates of the El Ideid-El Sodmein District, central Eastern Desert, Egypt: their metamorphism and petrogenetic implications
TL;DR: In this paper, backscattered electron images and electron microprobe analyses of chrome-spinels and associated silicates are made to evaluate their textural and compositional variations with metamorphism.
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Abu Hamamid Neoproterozoic Alaskan-type complex, south Eastern Desert, Egypt
E.S. Farahat,Hassan M. Helmy +1 more
TL;DR: Abu Hamamid (AH) Neoproterozoic (Sm/Nd model age of 770 ± 20 Ma) mafic-ultramafic intrusion lies along a NE-SW fracture zone in the Shadli Metavolcanic Belt, south Eastern Desert, Egypt as discussed by the authors.
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Post-collisional magmatism in the northern Arabian-Nubian Shield: The geotectonic evolution of the alkaline suite at Gebel Tarbush area, south Sinai, Egypt
E.S. Farahat,Mokhles K. Azer +1 more
TL;DR: The G. Tarbush alkaline suite most likely evolved via fractionation of mainly feldspar and minor mafic phases (hornblende, aegirine) from a common quartz syenite parental magma, which formed via partial melting of middle crustal rocks of the ANS juvenile crust as discussed by the authors.