Long-Range Correlations in the Diffuse Seismic Coda

By Michel Campillo, A. Paul. Science, 2003

1,266 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/00c43d68e5fdc69e6a43490669d7c691584b2890

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In Geophysics

Citations in the corpus

Tutorial on seismic interferometry: Part 1 — Basic principles and applications (2010, methodology): “Hence, in situations with few primary sources but many secondary sources only the late coda is used for Green's function retrieval Campillo and Paul (2003).”
Empirical synthesis of time-asymmetrical Green functions from the correlation of coda waves (2005, background): “The results of Campillo and Paul [2003] suggest that these different field-to-field correlations contain the different terms of the elastic Green tensor.”
Assessment of resolution and accuracy of the Moving Window Cross Spectral technique for monitoring crustal temporal variations using ambient seismic noise (2011, methodology): “…the cross-correlation of records of a random seismic wave field taken at various locati ns within a region of interest ⋆ MWCS: assessment of resolution and accuracy3 (Weaver & Lobkis 2001; Lobkis & Weaver 2001; Campillo & Paul 2003; Shapiro & Campillo 2004; Shapiro et al. 2005; Sabra et al. 2005).”
Extracting time‐domain Green's function estimates from ambient seismic noise (2005, background): “…t) by integration over the whole observation period T Cij 1; 2; tð Þ ¼ ZT 0 vi r1; tð Þvj r2; tþ tð Þdt: ð3Þ 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].”
Reconstructing Green's function by correlation of the coda of the correlation (C3) of ambient seismic noise (2008, background): “These waves have the expected properties for retrieving the Green’s functions [Lobkis and Weaver, 2001; Campillo and Paul, 2003].”
Frequency‐Bessel Transform Method for Effective Imaging of Higher‐Mode Rayleigh Dispersion Curves From Ambient Seismic Noise Data (2019, background): “After the pioneering works of Aki (1957) and other researchers (e.g., Campillo & Paul, 2003; Derode et al., 2003; Lobkis & Weaver, 2001; Sabra et al., 2005a, 2005b; Sánchez-Sesma et al., 2011; Shapiro & Campillo, 2004; Shapiro et al., 2005; Snieder, 2004), once useless ambient noise data were…”
Emergence of broadband Rayleigh waves from correlations of the ambient seismic noise (2004, positive): “Recently, the deterministic surface-wave Green functions has been extracted by the correlation of records of seismic coda of regional earthquakes in Mexico by Campillo and Paul [2003].”
Ambient noise Rayleigh wave tomography across Europe (2007, background): “Because they propagate in a region directly beneath Earth’s surface, surface waves typically generate better path coverage of the upper regions of Earth than body waves with the same distribution of seismic stations.”
P‐waves from cross‐correlation of seismic noise (2005, background): “…few years in various fields of wave physics such as ultrasonics [Weaver and Lobkis, 2001, 2004], underwater acoustics [Roux et al., 2004] and geophysics [Rickett and Claerbout, 1999; Campillo and Paul, 2003; Shapiro and Campillo, 2004; Wapenaar, 2004; Sabra et al., 2005a; Shapiro et al., 2005].”
A study of the seismic noise from its long-range correlation properties (2006, background): “seismic coda [Campillo and Paul, 2003] or seismic noise [Shapiro and Campillo, 2004] computed between a pair of distant stations contains, at least partially, the actual Green”
3‐D surface wave tomography of the Piton de la Fournaise volcano using seismic noise correlations (2007, positive): “We further normalize the data by disregarding completely the amplitudes and by keeping only a one-bit signal [ Campillo and Paul , 2003].”