Several occurrences of gold-bearing quartz veins are situated along the east–northeast-
trending Barramiya–Um Salatit ophiolitic belt in the central Eastern Desert of Egypt. In the …

Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) and Phased
Array L-band Synthetic Aperture Radar (PALSAR) images covering the Um Rus area in the …

Although gold production from orogenic deposits in the Arabian–Nubian Shield is currently
relatively minor, extensive alluvial and lode fields were exploited by the ancient Egyptians …

Serpentinized peridotite and associated listvenites of Neoproterozoic age outcrop in the Bir
Umq area of western Saudi Arabia. The mantle section of the Bir Umq ophiolite is …

Although associated with carbonatized/listvenitized ophiolites and thrust structures, the
morphology and internal structures of the auriferous quartz veins in the Haimur deposit …

ABSTRACT Most South Eastern Desert ophiolites are found along the Allaqi-Heiani-Gerf
suture along the Egypt-Sudan border. Serpentinites, altered slices of upper mantle, are the …

The ultramafic rocks of Gabal Balamhindit are exposed as conspicuous ridges in the south
Eastern Desert of Egypt, Northern Nubian Shield. These rocks include extensively to …

Ultramafic rocks exposed at the Earth's surface generally record multiple stages of evolution
that may include melt extraction, serpentinization, carbonatization, and metamorphism …

Gold-bearing quartz±carbonate veins at the El-Anbat mine area, in the South Eastern Desert
of Egypt, are associated with pervasively silicified, highly sheared ophiolitic and island arc …

The variably serpentinized mantle peridotites of the Late Neoproterozoic Ess ophiolite
(Western Saudi Arabia) are highly altered along shear zones and thrust planes to form …