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 …

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 …

Seismic interferometry is an exciting new field in geophysics utilizing multiple scattering
events to provide unprecedented views of the Earth's subsurface. This is the first book to …

The motion of a building depends on the excitation, the coupling of the building to the
ground, and the mechanical properties of the building. We separate the building response …

In passive seismic interferometry, new reflection data can be retrieved by crosscorrelating
recorded noise data. The quality of the retrieved reflection data is, among others, dependent …

Seismic interferometry, also known as Green's function retrieval by crosscorrelation, has a
wide range of applications, ranging from surface-wave tomography using ambient noise, to …

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 …

Seismic interferometry is a technique for estimating the Green's function that accounts for
wave propagation between receivers by correlating the waves recorded at these receivers …

With seismic interferometry one can retrieve the response to a virtual source inside an
unknown medium, if there is a receiver at the position of the virtual source. Using inverse …

To avoid the defocusing effects of propagating waves through salt and overburden with an
inaccurate overburden velocity model, we introduce a vertical seismic profiling (VSP) local …