Before the opening of the Red Sea, 30-25 Ma ago, the Arabian Shield
(650,000 km2) formed part of a larger geological ensemble, the Arabian-Nubian
Shield, which covers several countries, mainly Egypt, Eritrea, Ethiopia, Saudi Arabia,
Somalia, Sudan and Yemen. The Arabian-Nubian Shield consists primarily of Neoproterozoic
juvenile crust and represents an area of suturing between East and West Gondwana before
the Paleozoic. It formed through the accretion of numerous, mainly inter-oceanic, island
arcs along ophiolite-lined suture zones and gneissic fault zones between 900 Ma and 550 Ma
when the Mozambique ocean closed. |