Abstract The Bir Tuluha ophiolite is one of the most famous chromitite-bearing occurrences
in the Arabian Shield of Saudi Arabia, where chromitite bodies are widely distributed as …

Surface exposure of the Egyptian Precambrian basement complex covers ca. 100 000 km 2.
Outcrops of the basement rocks extend over extensive areas in southern Sinai, the Eastern …

To identify antimicrobial leads for medical applications, metabolites from the aerial part of
Artemisia herba-alba were extracted and chromatographically purified. Two new …

This paper details petrological and geochemical studies of an ultramafic–mafic intrusion in
the Southern Eastern Desert of Egypt. The Dahanib complex shows a concentric zonation …

The deep levels of Neoproterozoic island arcs are poorly known due to limited accessibility.
The Genina Gharbia Alaskan-type complex (south Eastern Desert, Egypt) is the remains of a …

The Happo-O'ne peridotite complex is situated in the northeastern part of the Hida Marginal
Tectonic Zone, central Japan, characterized by the high-P/T Renge metamorphism, and is …

Akarem Intrusion in the southern part of the Eastern Desert of Egypt is one of Alaskan-type
ultramafic-mafic complexes of the Neoproterozoic age. The olivine and pyroxene-rich …

The geodynamic settings of the Precambrian mafic–ultramafic complexes in the Eastern
Desert of Egypt have important bearing on understanding the geotectonic evolution of the …

The Ablah serpentinized peridotites and overlying layered metagabbros represent an
allochthonous piece of a dismembered ophiolite in the southern Hijaz terrane that belongs …

In Egypt, mafic-ultramafic complexes have been classified into three major types: incomplete
ophiolite sequences; Alaskan-type intrusions, concentrically-zoned bodies formed in a …