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- W1977758619 abstract "Abstract The complex major Allaqi shear zone occurs within the meta-volcanic and meta-sedimentary Neoproterozoic rocks of the central Wadi Allaqi and is important for our understanding of the development of the Arabian-Nubian Shield within the evolution of the East African (Pan-African) Orogeny (950—550 Ma). Early-formed northerly-facing complex thrust duplex systems, with attendant west-northwest—east-southeast orientated recumbent folds, dominate the area. Early ductile structural phases are superseded by more brittle structures, and the intrusion of four granitoid plutons punctuates the development history. The Allaqi shear zone is interpreted as the most northerly major dislocation of a fault-duplex zone of regional significance but an interpretation of the zone as a palaeo-suture is not proven despite the presence of an allochthonous ophiolitic unit (the Gebel Taylor Wedge), which has undergone blueschist-facies metamorphism." @default.
- W1977758619 created "2016-06-24" @default.
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- W1977758619 date "2001-08-01" @default.
- W1977758619 modified "2023-09-27" @default.
- W1977758619 title "Tectonic evolution of the Allaqi shear zone and implications for Pan-African terrane amalgamation in the south Eastern Desert, Egypt" @default.
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- W1977758619 doi "https://doi.org/10.1016/s0899-5362(01)80058-0" @default.
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