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 …

El Sibai gneissic complex, Central Eastern Desert, Egypt: folded nappes and syn-kinematic gneissic granitoid sheets–not a core complex

AR Fowler, H Khamees, H Dowidar - Journal of African Earth Sciences, 2007 - Elsevier
The El Sibai area of the Central Eastern Desert (CED) of Egypt consists of an ophiolitic
association of arc metavolcanics, ophiolitic rocks, mélange, metasediments and minor mafic …

Depositional styles of Early Ediacaran terrestrial volcanosedimentary succession in Gebel El Urf area, North Eastern Desert, Egypt

H Eliwa, C Breitkreuz, I Khalaf, K El Gameel - Journal of African Earth …, 2010 - Elsevier
Located 100km northwest of Hurghada, the volcanosedimentary successions of Gebel El Urf
is exposed between latitude 27° 45′ 30 ″and 27° 51′ 00 ″N and longitude 32° 49′ 00 …

Post-orogenic and anorogenic A-type fluorite-bearing granitoids, Eastern Desert, Egypt: petrogenetic and geotectonic implications

FH Mohamed, MM El-Sayed - Geochemistry, 2008 - Elsevier
The present study focuses on four A-type fluorite-bearing granitic plutons in the Eastern
Desert of Egypt which are classified into post-orogenic subsolvus (Homrit Waggat, 535Ma; …

Spectral analyses of basement rocks in El-Sibai-Umm Shaddad area, Central Eastern Desert, Egypt, using ASTER thermal infrared data

SM Hassan, MF Sadek, RO Greiling - Arabian Journal of Geosciences, 2015 - Springer
Abstract Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER)
level 1B (five thermal infrared (TIR) bands) data have been used to discriminate the exposed …

Magnetic fabrics and Pan-African structural evolution in the Najd Fault corridor in the Eastern Desert of Egypt

MM Abdeen, RO Greiling, MF Sadek… - Journal of African Earth …, 2014 - Elsevier
In order to assess the Pan-African structural evolution from early orogenic fabrics through
Najd wrenching to the latest orogenic collapse/extension, the authors used field work, aided …

Weathering of the peraluminous granite and their derived soils: a geochemical approach, Eastern Desert, Egypt

AE ElNagmy, MA Elhaddad, A Hemmdan… - Euro-Mediterranean …, 2024 - Springer
Samples for this study were collected from pristine granites and their surface-derived soils
from the Um Shaddad area, central Eastern Desert, Egypt. The elemental concentration was …

Geochemistry and geothermobarometry of the Um Eleiga Neoproterozoic island arc intrusive complex, SE Egypt: genesis of a potential gold-hosting intrusion

BA Zoheir, AM Mehanna… - Applied Earth Science, 2008 - journals.sagepub.com
Gabbro-diorite-tonalite±granodiorite complexes, derived from subduction-related, calc
alkaline magmas represent a distinct unit in the Precambrian basement of Egypt. These …

Geochemistry and petrogenesis of Pan-African late-to post-orogenic younger granitoids at Shalatin-Halaib, south Eastern Desert, Egypt

SA El-Nisr, MM El-Sayed, GM Saleh - Journal of African Earth Sciences, 2001 - Elsevier
The younger granitoids of the Shalatin-Halaib district in the south Eastern Desert of Egypt
are of syenogranite compositions. Based on petrological and geochemical studies, the …

The Role of Fractional Crystallization and Assimilationin the Evolution of the Zoned Mukhattata Pluton, Eastern Desert, Egypt

SA El-Nisr, MM El-Sayed - Geochemistry, 2002 - Elsevier
The zoned Mukhattata pluton, covering an area of about 25 km2, is composed of three
zones becoming more felsic towards the centre of the pluton (normal zoning). The most …