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 …
[图书][B] Surface wave methods for near-surface site characterization
Develop a Greater Understanding of How and Why Surface Wave Testing Works Using
examples and case studies directly drawn from the authors' experience, Surface Wave …
examples and case studies directly drawn from the authors' experience, Surface Wave …
Seismic interferometry and ambient noise tomography in the British Isles
H Nicolson, A Curtis, B Baptie, E Galetti - Proceedings of the Geologists' …, 2012 - Elsevier
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 …
identifiable, impulsive source of seismic energy, for example an earthquake or explosive …
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 …
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 …
Signal extraction using randomized-order multichannel singular spectrum analysis
Multichannel singular spectrum analysis (MSSA) is an effective algorithm for random noise
attenuation; however, it cannot be used to suppress coherent noise. This limitation results …
attenuation; however, it cannot be used to suppress coherent noise. This limitation results …
Ambient noise multimode Rayleigh and Love wave tomography to determine the shear velocity structure above the Groningen gas field
The Groningen gas field is one of the largest gas fields in Europe. The continuous gas
extraction led to an induced seismic activity in the area. In order to monitor the seismic …
extraction led to an induced seismic activity in the area. In order to monitor the seismic …
Mathematical morphological filtering for linear noise attenuation of seismic data
Linear coherent noise attenuation is a troublesome problem in a variety of seismic
exploration areas. Traditional methods often use the differences in frequency, wavenumber …
exploration areas. Traditional methods often use the differences in frequency, wavenumber …
Elastodynamic Green's function retrieval through single-sided Marchenko inverse scattering
The solution of the inverse scattering problem for the one-dimensional Schrödinger equation
is given by the Marchenko equation. Recently, a Marchenko-type equation has been derived …
is given by the Marchenko equation. Recently, a Marchenko-type equation has been derived …
6-C polarization analysis using point measurements of translational and rotational ground-motion: theory and applications
D Sollberger, SA Greenhalgh… - Geophysical Journal …, 2018 - academic.oup.com
We provide a six-component (6-C) polarization model for P-, SV-, SH-, Rayleigh-, and Love-
waves both inside an elastic medium as well as at the free surface. It is shown that single …
waves both inside an elastic medium as well as at the free surface. It is shown that single …