A discussion on the tectonic implications of Ediacaran late‐ to post‐orogenic A‐type granite in the northeastern Arabian Shield, Saudi Arabia

The transition from late‐orogenic to post‐orogenic magmatism following major orogenic episodes such as the Neoproterozoic to Cambrian East African Orogen (EAO) is an important, yet not well‐understood geological event marking the cessation of subduction‐controlled magmatism between buoyant lithospheric fragments. Forming the northern part of the EAO in the Arabian‐Nubian Shield are three granitic suites that successively intruded the same northeastern area and post‐date the ~640 Ma major orogenic episode: (1) 620–600 Ma alkali feldspar (hypersolvous) granite with alkaline/ferroan/A‐type geochemistry, (2) 599 Ma granite cumulates (some garnet‐bearing) with calc‐alkaline/magnesian affinities, and (3) 584–566 Ma alkali feldspar (hypersolvous) granite (aegirine‐bearing) with a distinctive peralkaline/ferroan/A‐type signature. Combining whole‐rock geochemistry from the southern and northern Arabian Shield, suites 1 and 2 are suggested to be products of late‐orogenic slab tear/rollback inducing asthenospheric mantle injection and lower crustal melting/fractionation toward A‐type/ferroan geochemistry. Suite 3, however, is suggested to be produced by post‐orogenic lithospheric delamination, which replaced the older mantle with new asthenospheric (rare earth element‐enriched) mantle that ultimately becomes the thermal boundary layer of the new lithosphere. Major shear zones, such as the 620–540 Ma Najd Fault System (NFS), are some of the last tectonic events recorded across the Arabian Shield. Data presented here suggest that the NFS is directly related to the late‐orogenic (620–600 Ma) slab tear/rollback in the northeastern Shield as it met with opposing subduction polarity in the southern Shield. Furthermore, this study infers that east and west Gondwana amalgamation interacted with opposing convergence reflected by the NFS. Key Points Three granites from the NE Arabian Shield post‐date a ~640 Ma major orogenic episode and record a change in mantle source Geochemical comparison suggests late‐orogenic lower crustal melting induced by slab tear followed by a switch to lithospheric delamination Late‐orogenic magmatism symbolizes an extensional phase of a major transpressional shear zone generated by opposing subduction polarity