During the late Cryogenian–Ediacaran (650–542Ma), the Arabian–Nubian Shield (ANS)
underwent final assembly and accretion to the Saharan Metacraton concurrent with the …

The Cadomian orogeny reflects S-directed subduction on the northern margin of Greater
Gondwana in Ediacaran–Cambrian time (∼ 600-500 Ma). It is well known from the eastern …

Alkaline (A-type and highly fractionated felsic I-type) granites that may have formed in post-
collisional plate tectonic environments are present in the Alaskan Cordillera, the New …

The assembly of the eastern part of Gondwana (eastern Africa, Arabian–Nubian shield
(ANS), Seychelles, India, Madagascar, Sri Lanka, East Antarctica and Australia) resulted …

We report C, Sr, and O isotopic as well as selected major and trace element data from Late
Proterozoic (ca. 540–900 Ma) marine carbonates in three widely separated basins. The …

Six distinctive tectonic episodes punctuate the stratigraphic record of the Gulf of Suez area.
These episodes include the Pan-African event (late Proterozoic), which resulted in the …

Deformational belts in the Arabian-Nubian Shield (ANS) are divided into:(1) those
associated with sutures, both arc-arc and arc-continental; and (2) post-accretionary …

Abstract The Arabian–Nubian Shield froms the suture between East and West Gondwana at
the northern end of the East African Orogen (EAO). The older components of the shield …

Samarium‐neodymium isotope systematics provide a means of determining the age of the
continental crust, where” age “refers to the amount of time the crustal rock material has been …

The Najd Fault System is a complex set of left‐lateral strike‐slip faults and ductile shear
zones that strike NW‐SE across the Precambrian of Arabia and Egypt. This system was …