K. Al-Toubi

TL;DR: In this article, the Gulf of Aden rift is considered to be a young ocean basin in which the earliest synrift to breakup structures are well exposed onshore and covered by thin sediment layers offshore.

TL;DR: In this article, surface heat-flow data from the Eastern Gulf of Aden indicate a thermal anomaly that has persisted after continental break-up, which may have been caused by small-scale convection that occurred during and after rifting.

TL;DR: In this article, the authors presented the results of the first probabilistic seismic hazard assessment (PSHA) in the framework of logic tree for Oman, where the earthquake catalogue was homogenized, declustered, and used to define seismotectonic source model that characterizes the seismicity of Oman.

TL;DR: In this article, the authors presented the results of the first probabilistic seismic hazard assessment (PSHA) in the framework of logic tree for Oman, where the earthquake catalogue was homogenized, declustered, and used to define seismotectonic source model that characterizes the seismicity of Oman.

TL;DR: In this paper, the authors apply a linear relationship between density and velocity to provide consistent density models from mid-crust down to about 250 km depth, and discuss the presence of partial melting in terms of interaction between the Sheba ridge melts and its along-axis segmentation.