The ophiolite melange of Wadi Dunqash and Wadi Arayis, Eastern Desert of Egypt: Petrogenesis and tectonic evolution. Acta Mineral.-Petrogr., XXXXVII, 129-141

Faculty Science Year: 1996
Type of Publication: ZU Hosted Pages:
Authors:
AbdelAal Mohammad AbdulKarim
Journal: Acta Mineralogica-Petrographica, Szaged Acta Mineralogica-Petrographica, Szaged Volume:
Keywords : , ophiolite melange , Wadi Dunqash , Wadi Arayis,    
Abstract:
Wadi Dunqash and Wadi Arayis in the central and southern Eastern Desert of Egypt are characterized by the presence of metamorphosed dismembered ophiolite sequence. This sequence consists of harzburgite- serpentinite, pyroxenite-chlorit
    
     
 
       

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Department Related Publications

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