One major cause of elastic wave attenuation in heterogeneous porous media is wave-
induced flow of the pore fluid between heterogeneities of various scales. It is believed that …

Traditionally, the Marchenko equation forms a basis for 1D inverse scattering problems. A
3D extension of the Marchenko equation enables the retrieval of the Green's response to a …

Traditional methods of imaging the Earth's subsurface using seismic waves require an
identifiable, impulsive source of seismic energy, for example an earthquake or explosive …

In the 1990s, the method of time-reversed acoustics was developed. This method exploits
the fact that the acoustic wave equation for a lossless medium is invariant for time reversal …

With the development of large networks, huge quantities of continuous recordings have
been made available. The extraction of deterministic information about the Earth structure …

The proliferation of seismic networks in Australia has laid the groundwork for high-resolution
probing of the continental crust. Here we develop an updated 3D shear-velocity model using …

Comprehensive observations of surface wave anisotropy across Alaska and the Aleutian
subduction zone would help to improve understanding of its tectonics, mantle dynamics, and …

Land seismic data are contaminated by surface waves (or ground roll). These surface waves
are a form of source-generated noise and can be strongly scattered by near-surface …

The Marchenko integral, key to inverse scattering problems across many disciplines, is a
long-standing equation that relates single-sided reflection data and Green's functions for …

Marchenko methods are based on integral representations which express Green's functions
for virtual sources and/or receivers in the subsurface in terms of the reflection response at …