Abstract The Red Sea is part of an extensive rift system that includes from south to north the
oceanic Sheba Ridge, the Gulf of Aden, the Afar region, the Red Sea, the Gulf of Aqaba, the …

The Betic Ophiolites consist of numerous tectonic slices, metric to kilometric in size, of
eclogitized mafic and ultramafic rocks associated to oceanic metasediments, deriving from …

As the Earth's best-known example of an active, incipient ocean basin, the Red Sea
provides crucial information about continental rifting and the tectonic transition from …

Intense analysis of geological, geophysical and particularly new available biostratigraphic
data from the Gulf of Suez (GS), Red Sea (RS) Gulf of Aqaba (GA) and the Eastern …

We present a new model of P-velocity anomalies in the upper mantle beneath the Arabian
Peninsula, Red Sea, and surrounding regions. This model was computed with the use of …

Abstract The Red Sea represents the most spectacular example of a juvenile ocean basin
on the modern Earth. Synthesis of regional aeromagnetic data, gravity data, seismic …

The Central Red Sea Rift is a natural laboratory to study the transition from rifting to
spreading. Based on new reflection seismic profiles and gravity modeling, we examined the …

In this study three new maps of Moho depths beneath the Arabian plate and margins are
presented. The first map is based on the combined gravity model, EIGEN 06C, which …

We present a new model of the stress state and present‐day tectonics of the Red Sea Rift
(RSR) based on an instantaneous geodynamic mantle flow model. The initial density and …

Rifts and rifted passive margins are often associated with thick evaporite layers, which
challenge seismic reflection imaging in the subsalt domain. This makes understanding the …