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• W2118008506 abstract "The structural pattern of the Gulf of Suez and Red Sea Rift is inherited from the basement tectonics. N140 faults (clysmic direction), parallel to the regional elongation of the rift, are associated with submeridian (Aqaba direction) and sub-E-W faults (Duwi direction) that also play an important role in the rifting processes. The pre-rift sedimentary cover includes Cretaceous and Eocene platform deposits. It was slightly deformed prior to rifting. The syn-rift sedimentary sequence comprises four major units (groups A to D) delimited by unconformities: Group A (Oligocene to Early Burdigalian), continental to restricted subaquatic deposits; Group B (Burdigalian to Middle Miocene), open marine sediments; Group C (Middle to Upper? Miocene), major evaporitic episode; and Group D (Plio-Pleistocene) which returns to an open marine environment. Four majors stages of structuration are recorded: an initial stage of compressive deformation (direction of shortening close to NW-SE) characterized by strike-slip movements and associated drag folds (early Group A); a tilted block stage (late Group A) corresponding to the period of highest extensional rate; a horst and graben stage (Group B) resulting in the cutting out of the tilted blocks by numerous synthetic faults; Group B corresponds to the period of highest subsidence rate when a flexuration stage of the margin, expressed by a centripetal evolution of the subsidence, is associated with major periferal uplift." @default.
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• W2118008506 date "1988-10-01" @default.
• W2118008506 modified "2023-10-10" @default.
• W2118008506 title "Tectonic and sedimentary evolution of the Gulf of Suez and the northwestern Red Sea" @default.
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• W2118008506 doi "https://doi.org/10.1016/0040-1951(88)90013-3" @default.
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