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العنوان
Structural Deformation of the Phanerozoic Sedimentary Succession of El-hamrawein Surrounding Areas, Northwest Red sea, Eastern Desert, Egypt /
المؤلف
Fheel, Amr Shaban Abdallah.
هيئة الاعداد
باحث / عمرو شعبان عبد الله فحيل
مشرف / محمد عاطف نوير
مناقش / مصطفى محمود يوسف
مناقش / يخيى عباس حامد القزاز
الموضوع
Geology.
تاريخ النشر
2014.
عدد الصفحات
p 108. :
اللغة
الإنجليزية
الدرجة
ماجستير
التخصص
الجيولوجيا
تاريخ الإجازة
15/12/2014
مكان الإجازة
جامعة طنطا - كلية العلوم * - جيولوجيا
الفهرس
Only 14 pages are availabe for public view

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from 134

Abstract

The mapped area is considered a part of rift system; this rift system was formed by the anticlockwise rotation of Arabian plate away from African plate about acoordinate pole of rotation in central or South-central Mediterranean Sea. The exposed rocks of Elhamrawein area are composed of more than 1300m. thick section of sedimentary succession rangr in age from late Cretaceous to recent. The oldest exposed rock units in the area belong to late cretaceous which divided into Nubia, Quseir,Duwi and Dakhla formations. The Paleocene is represented by Tarawn and Esna formations.