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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Ingratiate

,Timing of Extensional Faulting Along the Magma-Poor Central and Northern Red Sea Rift Margin—Transi despite evidence for asymmetric extension and hyperextended crust (Zabargad Island). An in-depth analysis of the timing, spatial distribution, and nature of Red Sea volcanism and its relationship to late Cenozoic extensional faulting should shed light on some of the misconceptions. Voluminous Eocen

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NOVA

Oceanization Starts at Depth During Continental Rupturing in the Northern Red Sea,ks recovered in the same area both from an oil well below a thick evaporitic-sedimentary sequence, and from a layered mafic complex exposed on the Brothers Islets. These new data provide constraints on the composition, depth of emplacement and age of early syn-rift magma intrusions into the deep cru

NOVA

Rifting and Salt Deposition on Continental Margins: Differences and Similarities Between the Red Seimentary basins formed during the Gondwana breakup. The interpretation of these seismic profiles integrated with gravity and magnetic potential field data suggest alternative models for the birth of oceanic basins that evolve from an earlier phase of intracontinental rift, salt deposition and contin

大包裹

Plate Motions Around the Red Sea Since the Early Oligocene,early Oligocene) and can be represented by two kinematic stages, characterized by distinct directions of extension and different duration. Deformation associated with rifting was accommodated through the reactivation of the inherited Proterozoic structures. We show that the first stage was character

myopia

Hydrothermal Prospection in the Red Sea Rift: Geochemical Messages from Basalts,measuring chlorine (Cl) excess in erupted lavas. The Red Sea Rift provides a unique opportunity to study assimilation of hydrothermally altered crust at an ultra-slow spreading ridge (maximum 1.6?cm?yr. full spreading rate) by Cl, due to its saline seawater (40–42‰, cf. 35‰ in open ocean water), the

Frenetic

,Salt Formation, Accumulation, and Expulsion Processes During Ocean Rifting—New Insight Gained from lt Walls’ and ‘Salt Ridges’), associated?with topographical lows (Deeps), suggest that the Red Sea currently?produces new volumes of brines and solid salts underground. The salt?producing zone is focused around the central rifting axis and?represents about 15% of the entire Red Sea area. The brines