The seismic signature of the Moho from which geologic and tectonic evolution hypotheses
are derived is to a large degree a result of the seismic methodology which has been used to …

This paper provides a review of array-based imaging techniques that use converted and
scattered teleseismic waves. It addresses various aspects of the imaging process, from the …

Seismic arrays, first introduced in the late 1950s to detect underground nuclear explosions,
have helped to improve our knowledge about the structure of the Earth for the last 40 years …

We demonstrate the feasibility of high-resolution seismic array imaging based on
teleseismic recordings using full numerical wave simulations. We develop a hybrid method …

We present a three‐dimensional (3‐D) hybrid method that interfaces the spectral‐element
method (SEM) with the frequency‐wave number (FK) technique to model the propagation of …

We present a novel 3-D pre-stack Kirchhoff depth migration (PKDM) method for teleseismic
receiver functions. The proposed algorithm considers the effects of diffraction, scattering and …

One of the current challenges faced by earthquake seismologists is the development of new
tools for high-resolution imaging of the lithosphere and underlying mantle. While …

Receiver function analysis is widely used to image sharp structures in the Earth, such as the
Moho or transition zone discontinuities. Standard procedures either rely on the assumption …

Information on fault zone structure is essential for our understanding of earthquake
mechanics, continental deformation and seismic hazard. We use the scattered seismic …

Imaging of tectonically complex regions can greatly benefit from dense network data and
resolution enhancement techniques. Conventional methods in the analysis of SS precursors …