Titlebook: Geological Setting, Palaeoenvironment and Archaeology of the Red Sea; Najeeb M.A. Rasul,Ian C.F. Stewart Book 2019 Springer Nature Switzer

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https://doi.org/10.1007/978-3-662-41325-8from orthogonal to oblique with respect to the Red Sea coastlines. Importantly, they correlate across the Red Sea, and provide piercing points for a near coast-to-coast palinspastic reconstruction of the Arabian and Nubian Plates along the entire Red Sea. A tight pre-rift fit of the Arabian and Nubi

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https://doi.org/10.1007/978-3-531-18892-8axial oceanic cells is either oceanic or it consists of melt-intruded extended continental crust). Gabbros show petrologic and geochemical signatures similar to those of MORB-type gabbroic cumulates and are compatible with their having been emplaced either in a continental or in an oceanic context.

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https://doi.org/10.1007/978-3-642-47406-4he proximal rifts onshore and in the platform. Basinward, more elusive features are characterized toward the transitional and oceanic crust in divergent margins. This work discusses alternative interpretations for syn-rift successions and salt distribution in regional seismic profiles from the Red S

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Die Ausnutzung minderwertiger Brennstoffe,e in the southern Red Sea and is still active in the northern region. In this time interval, an inherited system of NW–SE structures was reactivated as normal faults accommodating NE–SW extension, while NE–SW Proterozoic structures were reactivated as transfer strike–slip faults. Although no changes

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,Das Kochbuch und die neue Haushaltführung,). Although the stronger currents may help to maintain the upper channel morphology, it is unclear how they would have created the channel, nor can modern currents explain the deeper parts of the channel. The channel is straight and runs parallel with the spreading rift to the north, suggesting that