Petrology and geochemistry of the felsic dyke swarms in southwest Sinai, Egypt. Arab. Gulf Jour. Scient. Res., 13 (2), 239-257.

Faculty Science Year: 1995
Type of Publication: ZU Hosted Pages:
Authors:
Journal: Arab Gulf J. Scientific Res Arab Gulf J. Scientific Res Volume:
Keywords : Petrology , geochemistry , , felsic dyke swarms , southwest    
Abstract:
The southwestern part of Sinai massif is formed of Schists, gneisses and migmatites; metagabbro-diorite association and granitic rocks. They are dissected by dyke swarms of several different types, ages and styles, including mafic (old) an
   
     
 
       

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Department Related Publications

  • Shehta Abovendod Mohammed Hassan Eweda, "Clastic-carbonate sequence of Gabal El Safra , Sharm El Sheikh artea, southern Sinai, Egypt.", Egypt. J. Geol., 40/2: 805-844., 1996 More
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