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- W2023109403 abstract "The cratonisation of the Arabian Shield involved the accretion of ensimatic arc terranes in the west and south followed by continental collisions along the Nabitah and Al Amar sutures and the onset of the Najd strike-slip orogen. Volcanosedimentary successions which post-date these collisions have been proposed as the products of magmatism in transitional volcanic arcs. One such succession, the Bani Ghayy group, lies unconformably above a series of volcanosedimentary rocks associated with an older active continental margin and was deposited in three separate, elongate, fault-bounded grabens. Each graben contains coarse fanglomerate and fan delta deposits along the margin and proximal greywackes toward the centre. Reef limestones occur locally whereas volcanogenic rocks are widespread. The latter are geochemically bimodal and with the sediments are typical of continental rifting environments although deformed ultramafic rocks within internal reverse faults suggests that the grabens were floored, in part, by primitive mantle derived crust. Deposition of the Bani Ghayy group post-dates incipient motions along fractures of the Najd fault system. The orientation of the Bani Ghayy grabens and the geometry of the boundary faults are consistent with development in a regime of northwest-trending dextral shear. However, the Bani Ghayy grabens are displaced and deformed by later movements of the same faults but in a sinistral sense. Other successions correlated with the Bani Ghayy also preserve features consistent with deposition in continental grabens and the possibility that they represent arc volcanism is discounted." @default.
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- W2023109403 date "1986-04-01" @default.
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- W2023109403 title "The Bani Ghayy group; sedimentation and volcanism in pull-apart grabens of the Najd strike-slip orogen, Saudi Arabian shield" @default.
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- W2023109403 doi "https://doi.org/10.1016/0301-9268(86)90076-8" @default.
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