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- W2017948250 abstract "Abstract The cross structure (SW-NE) of the Gulf of Suez is well documented through several studies on the rifting in the area, whereas less emphasis has been placed on the structural interpretation along the axial direction of the rift itself. The aeromagnetic data show the presence of two main trends: “clysmic” (N320°) and “cross” trend (N50°). The reflection seismic profiles covering the Gulf of Suez offshore area indicate an alternance of ranges and asymmetrical basins in the axial direction as well as across the rift. Well data demonstrate the presence of structural dips either in NW or SE directions both in the pre-rifting and syn-rifting sedimentary sequences deposited in these asymmetrical basins. In an overall rifting tectonic framework, to explain the structural configuration resulting from the above data along the axial direction would imply a possible extension parallel to the axis of the rifting itself. This extension component occurs along the pre-existing cross trend oblique to the rifting, while the Aqaba trend does not seem to play any role. The axial extension has been active since the time of early rifting and it appears to have been reactivated in more recent times. In a plate tectonic framework, the axial extension of the Gulf of Suez area implies a movement of the Sinai microplate oblique to the axis of the rifting." @default.
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- W2017948250 date "1988-10-01" @default.
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- W2017948250 title "Possible axial extension in the Gulf of Suez rift (work hypothesis)" @default.
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