Seismic Interferometry: Tutorial on seismic interferometry: Part 1—Basic principles and applications
Seismic interferometry involves the crosscorrelation of responses at different receivers to
obtain the Green's function between these receivers. For the simple situation of an impulsive …
obtain the Green's function between these receivers. For the simple situation of an impulsive …
Green's function representations for seismic interferometry
K Wapenaar, J Fokkema - Geophysics, 2006 - library.seg.org
The term seismic interferometry refers to the principle of generating new seismic responses
by crosscorrelating seismic observations at different receiver locations. The first version of …
by crosscorrelating seismic observations at different receiver locations. The first version of …
[BOOK][B] Seismic interferometry
GT Schuster - 2009 - books.google.com
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 …
events to provide unprecedented views of the Earth's subsurface. This is the first book to …
Extracting Earth's elastic wave response from noise measurements
Recent research has shown that noise can be turned from a nuisance into a useful seismic
source. In seismology and other fields in science and engineering, the estimation of the …
source. In seismology and other fields in science and engineering, the estimation of the …
Application of surface-wave methods for seismic site characterization
Surface-wave dispersion analysis is widely used in geophysics to infer a shear wave
velocity model of the subsoil for a wide variety of applications. A shear-wave velocity model …
velocity model of the subsoil for a wide variety of applications. A shear-wave velocity model …
Tutorial on seismic interferometry: Part 2—Underlying theory and new advances
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 …
the fact that the acoustic wave equation for a lossless medium is invariant for time reversal …
Interferometry by deconvolution: Part 1—Theory for acoustic waves and numerical examples
I Vasconcelos, R Snieder - 2008 - pubs.geoscienceworld.org
Interferometry allows for synthesis of data recorded at any two receivers into waves that
propagate between these receivers as if one of them behaves as a source. This is …
propagate between these receivers as if one of them behaves as a source. This is …
Characterization of shallow geology by high-frequency seismic noise tomography
To study the applicability of the passive seismic interferometry technique to near-surface
geological studies, seismic noise recordings from a small scale 2-D array of seismic stations …
geological studies, seismic noise recordings from a small scale 2-D array of seismic stations …
Seismic interferometry, surface waves and source distribution
D Halliday, A Curtis - Geophysical Journal International, 2008 - academic.oup.com
Seismic interferometry can be used to estimate interreceiver surface wave signals by cross-
correlation of signals recorded at each receiver. The quality of the estimated surface waves …
correlation of signals recorded at each receiver. The quality of the estimated surface waves …
Virtual seismometers in the subsurface of the Earth from seismic interferometry
The Earth's interior can be imaged by analysing the records of propagating seismic waves.
However, the global array of permanent seismometers that record seismic energy is …
However, the global array of permanent seismometers that record seismic energy is …