The tectonic evolution of the Arabian–Nubian Shield (ANS), the northern continuation of the
East African Orogen (EAO), is enigmatic and a matter of controversy. The EAO is observed …

Satellite-based multi-sensor data coupled with field and microscopic investigations are used
to unravel the setting and controls of gold mineralization in the Wadi Beitan–Wadi Rahaba …

This paper presents a new approach to modelling flash floods in dryland catchments by
integrating remote sensing and digital elevation model (DEM) data in a geographical …

Kadabora-Suwayqat area, in the Central Eastern Desert of Egypt, is built up by a wide
variety of non-consanguineous, basement rock units, which represent a tectono-stratigraphic …

Intensive investigation of the basement rock units of Abu Marawat-Semna area in the
northern part of Central Eastern Desert of Egypt and their gold-bearing alteration zones …

Abstract The Wadi Ghadir area, Central Eastern Desert, Egypt is covered by a sequence of
Pan-African basement rocks comprising allochthonous ophiolitic rock assemblage thrust …

Enormous quantities of practically untapped talc–magnesite rocks are distributed in the
Wadi Barramiya area in intimate spatial and genetic association with the ophiolitic …

Detailed field mapping and structural studies of the area around the mouth of Wadi Hodein,
some 20km west of Shalatein at the Red Sea coast in the south Eastern Desert of Egypt …

A variety of Late Neoproterozoic gneisses and amphibolites are distributed along the N–S
trending Hamisana Shear Zone (HSZ), in southeastern Egypt. The HSZ originated after the …

Groundwater constitutes the main source of freshwater in Shalatein, on the western coast of
the Red Sea, in Egypt. The fresh aquifer of Shalatein is intensively dissected by shallow and …