The Umm Gheig Formation belongs to the Abu Ziran Group of the Central Eastern Desert of Egypt. Rocks of this formation are originally derived from basalt, andesite and subordinate rhyolite. Although the formation includes two pétrographie associations suffering different grades of metamorphism, however, they have close consanguineous magmatic relationship. It is suggested that these associations belonging to tholeiitic magma type which are tectonically emplaced as island arc
The basement rocks of the Eastern Desert of Egypt represent a Proterozoic eugeosynclinal system. Thi...
The Neoproterozoic rocks of the Bir Madi area, south eastern desert, comprise a Metagabbro-Diorite C...
The Abu Dabbab albite granite (ADAG), in the central Eastern Desert of Egypt, hosts the most signifi...
The petrography of the Precambrian iron-bearing formation at Wadi Kareim proved that the formation c...
The geochemistry of the ophiolitic complexes and younger late orogenic sedimentary rocks in the Wadi...
A thesis submitted to the Faculty of Science & Computing, University of Luton, in partial fulfilment...
The present work is a geologieal, structural and geochemieal study on the Pan-African basement rocks...
The Samadai granitic complex in the Central Eastern Desert of Egypt is petrochemically evaluated. Ma...
The Gabal* Meatiq area was studied geologically and petrographically in detail by several workers. T...
The dyke swarms in southwestern Sinai consist of mafic (old) and felsic (young) suites. The mafic on...
Younger granite bodies form two arches, the western and the eastern (WA, EA), which extend from the ...
The present monograph by A.A. Rashwan is a major contribution to the Bilateral Cooperation in Geosci...
The ophiolitic rocks, island arc metasediments, and granitic rocks are encountered in the study of t...
Tow mica granites of the Abu Rusheid - Eir Arib district in the Southeastern Desert of Egypt, cut pr...
Banded iron formation (BIF) is exposed among the Precambrian rocks in the Wadi Karim and Um Anab are...
The basement rocks of the Eastern Desert of Egypt represent a Proterozoic eugeosynclinal system. Thi...
The Neoproterozoic rocks of the Bir Madi area, south eastern desert, comprise a Metagabbro-Diorite C...
The Abu Dabbab albite granite (ADAG), in the central Eastern Desert of Egypt, hosts the most signifi...
The petrography of the Precambrian iron-bearing formation at Wadi Kareim proved that the formation c...
The geochemistry of the ophiolitic complexes and younger late orogenic sedimentary rocks in the Wadi...
A thesis submitted to the Faculty of Science & Computing, University of Luton, in partial fulfilment...
The present work is a geologieal, structural and geochemieal study on the Pan-African basement rocks...
The Samadai granitic complex in the Central Eastern Desert of Egypt is petrochemically evaluated. Ma...
The Gabal* Meatiq area was studied geologically and petrographically in detail by several workers. T...
The dyke swarms in southwestern Sinai consist of mafic (old) and felsic (young) suites. The mafic on...
Younger granite bodies form two arches, the western and the eastern (WA, EA), which extend from the ...
The present monograph by A.A. Rashwan is a major contribution to the Bilateral Cooperation in Geosci...
The ophiolitic rocks, island arc metasediments, and granitic rocks are encountered in the study of t...
Tow mica granites of the Abu Rusheid - Eir Arib district in the Southeastern Desert of Egypt, cut pr...
Banded iron formation (BIF) is exposed among the Precambrian rocks in the Wadi Karim and Um Anab are...
The basement rocks of the Eastern Desert of Egypt represent a Proterozoic eugeosynclinal system. Thi...
The Neoproterozoic rocks of the Bir Madi area, south eastern desert, comprise a Metagabbro-Diorite C...
The Abu Dabbab albite granite (ADAG), in the central Eastern Desert of Egypt, hosts the most signifi...