Geotectonic significance of the Neoproterozoic ophiolitic metagabbros of Muiswirab area, South Eastern Desert, Egypt: constraints from their mineralogical and geochemical characteristics

Author:

Mogahed Moustafa M.ORCID,Saad Wlaa Mahmoud

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Reference156 articles.

1. Abd El-Rahman YA, Polat A, Dilek Y, Fryer BJ, El-Sharkawy M, Sakran S (2009) Geochemistry and tectonic evolution of the Neoproterozoic incipient arc–forearc crust in the Fawakhir area, Central Eastern Desert of Egypt. Precambrian Res 175:116–134

2. Abdel Aal A, Farahat E, Hoinken G, El-Mahalawi M (2003) Ophiolites from the Egyptian Shield: a case for a possible inter-arc origin. Mitt Oesterr Ges 148:81–83

3. Abdel-Karim A-AM, Ahmed Z (2010) Possible origin of the ophiolites of Eastern Desert, Egypt, from geochemical perspectives. Arab J Sci Eng 35:115

4. Abdel-Karim A-AM, Ali S, El-Shafei SA (2018) Mineral chemistry and geochemistry of ophiolitic metaultramafics from Um Halham and Fawakhir, Central Eastern Desert, Egypt. Int J Earth Sci 107:2337–2355

5. Abu El Farh M (2004) A comparative study based on petrography geochemistry of the granitoids in Hafafit area environs, Eastern Desert, Egypt. Ph.D. Dissertation. Suez Canal University, p 169

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