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This paper presents a kinematic model for the development of marginal extensional half-graben sub-basins in the northern Red Sea and Gulf of Suez rift zones, utilizing Landsat ETM+ and structural data. The model outlines the evolution of the rift system from late Oligocene to early Miocene, detailing the processes of oblique rifting and the formation of antithetic faults. It highlights the role of pre-existing structures in shaping the rift segments and the current phase of rifting influenced by the Dead Se

Author

mostafa nagy

Language

EN