Emergence of broadband Rayleigh waves from correlations of the ambient seismic noise

By N. M. Shapiro, Michel Campillo. 2004

1,451 citations recorded by the source corpus.

Subfields: Geophysics, Ocean Engineering

View Paper: https://www.semanticscholar.org/paper/93a33e93c70c12146e713b0ce6e87f1cf8c9cb2b

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Citations in the corpus

Spurious multiples in seismic interferometry of primaries (2006, background): “, 2004], in crustal seismology for the retrieval of the surface wave Green’s function [Campillo and Paul, 2003; Shapiro and Campillo, 2004; Shapiro et al., 2005],”
Transdimensional inversion of receiver functions and surface wave dispersion (2012, methodology): “…to invert RFs jointly with observations based on the cross-correlation of ambient noise recorded at nearby receivers [Campillo and Paul, 2003; Shapiro and Campillo, 2004; Stehly et al., 2009], which 3 of 24 provides apparent travel times of surface waves at periods 1–30 s (mostly sensitive…”
Extracting time‐domain Green's function estimates from ambient seismic noise (2005, methodology): “Several researchers have used a form similar to equation (1), but instead of the derivative they used the cross correlation [e.g., Campillo and Paul, 2003; Shapiro and Campillo, 2004 ].”
Origin of deep ocean microseisms by using teleseismic body waves (2010, methodology): “Application of this principle to large amount of continuous digital seismic records provided by modern networks provides us with new approaches for seismic tomography [e.g., Shapiro and Campillo, 2004; Shapiro et al., 2005; Sabra et al., 2005; Yang et al., 2007; Stehly et al., 2009] and monitoring”
Sudden drop of seismic velocity after the 2004 Mw 6.6 mid-Niigata earthquake, Japan, observed with Passive Image Interferometry (2009, methodology): “Using this method, the elastic Green’s function between two seismometers is constructed as a first step using the cross correlation of seismic noise recorded at the two sensors [ Shapiro and Campillo, 2004; Shapiro et al., 2005].”
Determination of surface‐wave phase velocities across USArray from noise and Aki's spectral formulation (2009, methodology): “…of background ground motion for pairs of stations has recently been shown to be a powerful method for determining interstation surface-wave group and phase velocities [Shapiro and Campillo, 2004; Sabra et al., 2005; Shapiro et al., 2005; Yao et al., 2006; Bensen et al., 2007; Lin et al., 2008].”
Empirical synthesis of time-asymmetrical Green functions from the correlation of coda waves (2005, background): “Shapiro and Campillo [2004] have shown that coherent broadband dispersive wave trains emerge from the cross correlation of ambient seismic noise records between stations many hundred kilometers apart and that dispersion curves can be measured in the absence of earthquake records.”
The origin of deep ocean microseisms in the North Atlantic Ocean (2007, background): “The seismic background noise dominated by oceanic microseisms can be effectively used as a seismic source for tomographic studies of geological properties of the Earth’s crust (Shapiro & Campillo 2004; Shapiro et al. 2005; Weaver 2005; Ritzwoller et al. 2006; Stehly et al. 2006).”
Processing seismic ambient noise data to obtain reliable broad-band surface wave dispersion measurements (2007, methodology): “…on crosscorrelations between pairs of stations have confirmed the theory for surface waves using both coda waves (Campillo & Paul 2003; Paul et al. 2005) and long ambient noise sequences (Shapiro & Campillo 2004; Sabra et al. 2005a) and for crustal body waves using ambient noise (Roux et al. 2005).”
Seismic tomography with the reversible jump algorithm (2009, background): “The use of ambient seismic noise to recover the traveltimes of surface waves between pairs of stations is rapidly becoming popular (Shapiro & Campillo 2004).”
Structure of young East Pacific Rise lithosphere from ambient noise correlation analysis of fundamental- and higher-mode Scholte-Rayleigh waves (2011, methodology): “…or coda-wave cross-correlation has been used to estimate surface-wave propagation (Green’s functions) between receivers (Campillo and Paul, 2003; Shapiro and Campillo, 2004), and therefore has been widely used for surface-wave tomography to investigate crustal structure all over the world…”