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- W1548717824 abstract "Abstract We establish the kinematics of the rotation of Arabia with respect to Africa and show that the rotation rate of Africa increased by a factor of about four in late Serravallian time, about 12–13 Ma ago. We discuss evidence that oceanic accretion started simultaneously in the Gulf of Aden and in the Red Sea at this time. It is also at this time that the Levant and Anatolian fault systems were initiated. Our initial reconstruction of the Red Sea Rift in Late Oligocene-Early Miocene time approximately superposes the present shore lines which coincide with the mid-point of the zones of rapid crustal thinning, the future continental slopes. The amount of extension during the early phase of continental rifting is obtained by assuming that the total volume of continental crust is conserved during extension, and by checking these estimates through closure around the Sinai triple junction. In the Late Miocene, the Southern evant fault zone was a zone of distributed shear deformation, through counterclockwise block rotation, extending soul h ward within the northernmost Red Sea. Since the Early Pliocene, the shear motion has been localized within the Gulf of Aqaba, changing the tectonic pattern in the northern Red Sea." @default.
- W1548717824 created "2016-06-24" @default.
- W1548717824 creator A5021218088 @default.
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- W1548717824 date "1988-10-01" @default.
- W1548717824 modified "2023-09-30" @default.
- W1548717824 title "The rotation of Arabia and the Levant fault system" @default.
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- W1548717824 doi "https://doi.org/10.1016/0040-1951(88)90020-0" @default.
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