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The pre-Pan-African deformed granite cycle of the Gabal El-Sibai swell, Eastern Desert, Egypt

The Gabal El-Sibai area is a structural high in which variably deformed granites and gneisses are structurally exposed underneath an overthrusted Pan-African ophiolitic melange and intruded by undeformed Pan-African granites. The deformed granites constitute a complete granite cycle starting with au...

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Main Authors: Khudeir, Ali Abdelkader Abdalla (Author) , Ǧabī, Samīr al- (Author) , El-Din, Gamal Kamal (Author) , Asran, Asran M. H. (Author) , Greiling, Reinhard O. (Author)
Format: Article (Journal)
Language:English
Published: 1995
In: Journal of African earth sciences
Year: 1995, Volume: 21, Issue: 3, Pages: 395-406
ISSN:1879-1956
DOI:10.1016/0899-5362(95)00095-B
Online Access:Verlag, lizenzpflichtig, Volltext: https://doi.org/10.1016/0899-5362(95)00095-B
Verlag, lizenzpflichtig, Volltext: https://www.sciencedirect.com/science/article/pii/089953629500095B
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Author Notes:Ali A. Khudeir, Samir El-Gaby, Gamal Kamal El-Din, Asran M.H. Asran, Reinhard O. Greiling

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520 |a The Gabal El-Sibai area is a structural high in which variably deformed granites and gneisses are structurally exposed underneath an overthrusted Pan-African ophiolitic melange and intruded by undeformed Pan-African granites. The deformed granites constitute a complete granite cycle starting with autochthonous to parautochthonous, calc-alkaline I-type granites and ending with post-tectonic, within-plate alkaline granites. They indicate that the Sibai infrastructure represents a pre-Pan-African continental crust incorporated in the Pan-African orogenic belt. - Résumé - La région du Gabal El-Sibai est un relief structural positif composé de granites et de gneiss déformés de manière variable. Ces derniers sont situés structuralament sous un mélange ophiolitique pan-african charrié et sont intrudés par des granites pan-africains non déformés. Les granites déformés constituent un cycle granitique complet débutant avec des granites calco-alcalins de type I autochtones à parautochtones et se terminant avec des granites alcalins post-tectoniques intra-plaques. Ils indiquent que l'infrastructure de Sibai représente une croûte continentale pré-pan-africaine incorporée dans la chaîne orogénique pan-africaine. 
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