Through various scales of observation, ranging from remote sensing data, field investigations, hand specimens, microscopic petrographic examinations, XRD, to SEM …
The Neoproterozoic tectonic evolution of the Egyptian Eastern Desert (EED) basement is documented, principally through its history of structural events, and to a lesser degree …
Abstract The Precambrian crust of Africa comprises large remnants of Archaean massifs, which are parts of even larger units, some of which were subjected to tectonic reactivation in …
H de Wall, RO Greiling, MF Sadek - Precambrian Research, 2001 - Elsevier
The Hamisana zone (HZ) is one of the major high strain zones of the Pan-African (Neoproterozoic) Arabian–Nubian shield (ANS). It trends broadly N–S from northern Sudan …
AR Fowler, B El Kalioubi - Tectonophysics, 2002 - Elsevier
The Wadi Hafafit Complex (WHC) is an arcuate belt of orthogneisses, migmatites and other high-grade metamorphic rocks, which marks the boundary between the Central Eastern and …
A Shalaby - Journal of African Earth Sciences, 2010 - Elsevier
Although the gneissic domes in Eastern Desert of Egypt have been studied recently in a considerable detail; their origin remains controversial. Basically four schools of thought exist …
RO Greiling, H De Wall, MF Sadek, C Dietl - Journal of African Earth …, 2014 - Elsevier
Field investigations, microstructural observations, and magnetic fabric analyses revealed a polyphase, late Pan-African deformational evolution in the Um Sheqila–Um Had (595 Ma) …
MA Obeid, AM Hussein, MA Abdallah - Applied Earth Science, 2001 - Taylor & Francis
Abstract The El Beida area of the Eastern Desert, Egypt, comprises a wide variety of Late Proterozoic rocks. It is occupied by ophiolitic serpentinites, metagabbros and pillow …
AL Abdeldayem, Z Hamimi - The Geology of the Egyptian Nubian Shield, 2021 - Springer
Abstract The Pan-African belt (PAB) of Egypt outcrops mainly in the Eastern Desert and Southern Sinai. It occupies the northwestern sector of the Arabian-Nubian Shield (ANS) and …