Phase and Correlation in `Random' Seismic Fields and the Reconstruction of the Green Function

By Michel Campillo. 2004

197 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/f9d88a941e18535b5180e76cabad3ffa48e3ac71

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In Geophysics

Citations in the corpus

A study of the seismic noise from its long-range correlation properties (2006, background): “…expected to be nearly symmetric in amplitude and in arrival time with its positive and negative parts corresponding to the Green function of the medium and its anticausal counterpart, respectively [e.g., Lobkis and Weaver, 2001; Van Tiggelen, 2003; Snieder, 2004; Sánchez-Sesma and Campillo, 2006].”
Tomography of the Alpine region from observations of seismic ambient noise (2009, background): “(Weaver & Lobkis, 2001; Lobkis & Weaver, 2001; Colin de Verdière, 2006a; Colin de Verdière, 2006b; Sánchez-Sesma et al., 2006a; Sánchez-Sesma et al., 2006b; Larose et al., 2006; Campillo, 2006).”
Anelastic Earth structure from the coherency of the ambient seismic field (2008, methodology): “[61] As explained by Sánchez-Sesma and Campillo [2006] the relation arises from the fact that the imaginary part of the frequency domain Green’s function for Rayleigh waves has the shape of a Bessel function in a homogeneous medium.”
Traveltime measurements from noise correlation: stability and detection of instrumental time-shifts (2007, background): “…been recently shown that the time cross-correlation function of seismic ambient noise (Shapiro & Campillo 2004) computed between a pair of distant stations contains, at least partially, the actual Green’s function between the two stations (Campillo 2006; Larose et al. 2006, and references therein).”
Reconstructing Green's function by correlation of the coda of the correlation (C3) of ambient seismic noise (2008, background): “Reviews on the correlation of seismic noise and coda waves are given by Campillo [2006] , Larose et al. [2006], and Goue´dard et al. [2008].”
3‐D surface wave tomography of the Piton de la Fournaise volcano using seismic noise correlations (2007, unknown): “In seismology, recent studies also showed that the Rayleigh wave Green’s function between pairs of seismographs can be extracted from cross-correlations of coda waves and ambient noise [Shapiro and Campillo, 2004; [Campillo, 2006].”