Deforming belts in the Arabian‐Nubian Shield (ANS) are classified into (1) suture‐related belts, including arc–arc and arc‐continental, and (2) post‐accretionary systems, including N …
Geological, geochronological and isotopic data are integrated in order to present a revised model for the Neoproterozoic evolution of Western Gondwana. Although the classical …
Neoproterozoic crust is beautifully exposed in the Eastern Desert (ED) of Egypt as an unbroken rift-flank uplift extending∼ 800 km between the Nile and the Red Sea, from near …
Abstract The Arabian-Nubian Shield (ANS) underwent a regional carbonation event with CO 2 fluxes derived from the mantle and circulated along post-accretionary shear zones, thus …
Abstract Korab Kansi and Abu Dahr Neoproterozoic ophiolitic peridotites in the Southern Eastern Desert (SED) of Egypt, are parts of the largest ophiolitic nappes in the Arabian …
AAM Abdel-Karim, S Ali, HM Helmy, SA El-Shafei - Lithos, 2016 - Elsevier
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 …
S Ali, T Ntaflos, M Sami - Geochemistry, 2021 - Elsevier
Abstract Serpentinites in the Eastern Desert of Egypt are the most distinctive lithological unit in the Arabian–Nubian Shield (ANS) ophiolite sequence which associated with major suture …
RJ Stern, K Ali - The geology of Egypt, 2020 - Springer
Precambrian basement of the Egyptian sector of the Arabian-Nubian Shield are well exposed on the flanks of the Red Sea and along the border with Sudan, making it an …