The Arabian Plate originated∼ 25Ma ago by rifting of NE Africa to form the Gulf of Aden and
Red Sea. It is one of the smaller and younger of the Earth's lithospheric plates. The upper …

The goal of this paper is to provide an overview of the current state of the art in seismic
tomography, and trace its origins from pioneering work in the early 1970s to its present …

We present a novel method for joint inversion of receiver functions and surface wave
dispersion data, using a transdimensional Bayesian formulation. This class of algorithm …

A non-linear Bayesian Monte-Carlo method is presented to estimate a Vsv model beneath
stations by jointly interpreting Rayleigh wave dispersion and receiver functions and …

We investigate mantle plumes and associated flow beneath the lithosphere by imaging the
three-dimensional S-velocity structure beneath Arabia and East Africa. This image shows …

We have constructed a 3-D shear wave velocity (Vs) model for the crust and uppermost
mantle beneath the Middle East using Rayleigh wave records obtained from ambient-noise …

Abstract Earth Crustal Model 1 (ECM1) is a 1° x 1° global crustal model that describes the
thickness of the crust, including the overlying sediments, and the corresponding seismic …

We collected and processed a large amount of high‐quality broadband teleseismic
waveform data recorded by the 48 Chinese National Digital Seismic Network stations to …

We study the lithospheric structure of Africa, Arabia and adjacent oceanic regions with
fundamental-mode surface waves over a broad period range. Including group velocities with …

Receiver functions are a powerful tool to isolate and interpret receiver-side structure effects
in teleseismic seismic records. They are easily constructed by deconvolving one component …