Neoproterozoic (835–720 Ma) serpentinites in the Eastern Desert, Egypt: fragments of forearc mantle
Most Neoproterozoic ophiolites of the Arabian-Nubian Shield show compositions consistent
with formation in a suprasubduction zone environment, but it has not been clear whether this …
with formation in a suprasubduction zone environment, but it has not been clear whether this …
A fore-arc setting of the Gerf ophiolite, Eastern Desert, Egypt: evidence from mineral chemistry and geochemistry of ultramafites
The Gerf ophiolite is the largest mantle-derived complex in the Arabian–Nubian Shield
(ANS). This ophiolitic complex extends for tens of kilometers in the south Eastern Desert …
(ANS). This ophiolitic complex extends for tens of kilometers in the south Eastern Desert …
Petrogenetic evolution of the Neoproterozoic igneous rocks of Egypt
Abstract The Late Neoproterozoic basement exposures in the Sinai Peninsula and Eastern
Desert of Egypt represent the northern part of the Nubian Shield, which was contiguous with …
Desert of Egypt represent the northern part of the Nubian Shield, which was contiguous with …
Multiple stages of carbonation and element redistribution during formation of ultramafic-hosted magnesite in Neoproterozoic ophiolites of the Arabian-Nubian Shield …
We present a study of the serpentinized peridotites of the Ghadir-Mohagar-Ambaut area,
Egypt. They represent the mantle section of a dismembered ophiolite, tectonically emplaced …
Egypt. They represent the mantle section of a dismembered ophiolite, tectonically emplaced …
Supra-subduction affinity in the Neoproterozoic serpentinites in the Eastern Desert, Egypt: evidence from mineral composition
AES Khalil, MK Azer - Journal of African Earth Sciences, 2007 - Elsevier
Serpentinites in the Eastern Desert (ED) of Egypt represent integral components of the
ophiolites. Metamorphic textures of the serpentinites preserve the complex mineralogical …
ophiolites. Metamorphic textures of the serpentinites preserve the complex mineralogical …
Neoproterozoic Ophiolites of the Arabian-Nubian Shield
Abundant ophiolites are distinctive components of the Arabian-Nubian Shield (ANS),
providing important clues about its origin and hosting many of its valuable mineral …
providing important clues about its origin and hosting many of its valuable mineral …
Petrological studies of Neoproterozoic serpentinized ultramafics of the Nubian Shield: spinel compositions as evidence of the tectonic evolution of Egyptian ophiolites
MK Azer - Acta Geologica Polonica, 2014 - geojournals.pgi.gov.pl
The mafic-ultramafic rocks of the Gabal El-Degheimi area, Central Eastern Desert of Egypt,
are parts of an ophiolitic section. The ophiolitic rocks are dismembered and tectonically …
are parts of an ophiolitic section. The ophiolitic rocks are dismembered and tectonically …
Mineralogy and chemical aspects of some ophiolitic metaultramafics, central Eastern Desert, Egypt: Evidences from chromites, sulphides and gangues
AAM Abdel‐Karim, SA El‐Shafei - Geological Journal, 2018 - Wiley Online Library
Chromites and sulphides are the most common ore minerals in the ophiolitic metasomatized
ultramafics (~ 790 Ma) of Um Halham, Fawakhir and Barramiya, central Eastern Desert …
ultramafics (~ 790 Ma) of Um Halham, Fawakhir and Barramiya, central Eastern Desert …
Pan-African (intraplate and subduction-related?) metasomatism in the Fawakhir ophiolitic serpentinites, Central Eastern Desert of Egypt: mineralogical and …
Fawakhir serpentinites are the most western ophiolitic ultramafics relative to the Pan-African
collision suture at the Qift-Quseir road in the Central Eastern Desert of Egypt. Their location …
collision suture at the Qift-Quseir road in the Central Eastern Desert of Egypt. Their location …
Spinels, Fe–Ti oxide minerals, apatites, and carbonates hosted in the ophiolites of Eastern Desert of Egypt: mineralogy and chemical aspects
Abstract Spinels, Fe–Ti oxide minerals, apatites, and carbonates hosted in ophiolitic
serpentinites and metagabbros of Gabal Garf (southern ED) and Wadi Hammariya (central …
serpentinites and metagabbros of Gabal Garf (southern ED) and Wadi Hammariya (central …