Suture (s) and major shear zones in the Neoproterozoic basement of Egypt

Z Hamimi, MA Abd El-Wahed - The Geology of Egypt, 2020 - Springer
Abstract The Arabian-Nubian Shield (ANS), the northern extension of the East African
Orogen (EAO), consists of a number of amalgamated island-arc tectonic terranes, separated …

[HTML][HTML] Multiscale mineralogical investigations for mineral potentiality mapping of Ras El-Kharit-Wadi Khashir district, Southern Eastern Desert, Egypt

HM El-Desoky, A Shebl, AM Abdel-Rahman… - The Egyptian Journal of …, 2022 - Elsevier
Through various scales of observation, ranging from remote sensing data, field
investigations, hand specimens, microscopic petrographic examinations, XRD, to SEM …

Structural and tectonic framework of Neoproterozoic basement of Egypt: from gneiss domes to transpression belts

AR Fowler, Z Hamimi - The geology of Egypt, 2020 - Springer
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 …

The metamorphism and deformation of the basement complex in Egypt

B El Kalioubi, AR Fowler, K Abdelmalik - The Geology of Egypt, 2020 - Springer
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 …

Post-collisional shortening in the late Pan-African Hamisana high strain zone, SE Egypt: field and magnetic fabric evidence

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 …

The Migif–Hafafit gneissic complex of the Egyptian Eastern Desert: fold interference patterns involving multiply deformed sheath folds

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 …

The northern dome of Wadi Hafafit culmination, Eastern Desert, Egypt: structural setting in tectonic framework of a scissor-like wrench corridor

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 …

Late Pan-African granite emplacement during regional deformation, evidence from magnetic fabric and structural studies in the Hammamat–Atalla area, Central …

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) …

Shear zone-hosted gold mineralization in the Late Proterozoic rocks of El Beida area, south Eastern Desert, Egypt

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 …

Application of Magnetic Susceptibility and Its Anisotropy in Deciphering the Tectonic Evolution of the Pan-African Belt of Egypt

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 …