Empirical synthesis of time-asymmetrical Green functions from the correlation of coda waves

By A. Paul, Michel Campillo, L. Margerin, É. Larose, A. Derode. 2005

186 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/8b161ea0f071bc852fa152118fed804bd4d2ba57

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In Geophysics

Citations in the corpus

Ambient noise Rayleigh wave tomography of New Zealand (2007, result): “These observations are consistent with oceanographic data, which reveal that the highenergy west, south and east coasts of New Zealand have predominant wave heights and periods of 1–3 m and 6–8 s, ∼4 m and 10–12 s, and 0.5–2 m and 7–11 s, respectively (Pickrill & Mitchell 1979).”
Reconstructing Green's function by correlation of the coda of the correlation (C3) of ambient seismic noise (2008, background): “It is of particular noteworthiness here that some have correlated seismic coda with a degree of success [Campillo and Paul, 2003; Paul et al., 2005].”
Surface-wave array tomography in SE Tibet from ambient seismic noise and two-station analysis: I - Phase velocity maps (2006, unknown): “…functions, which are by deﬁnition reciprocal and independent of the seismic source, the EGFs that are estimated from actual coda waves or ambient seismic noise may be time asymmetrical due to the inhomogeneous distribution of noise sources and attenuation (Paul et al. 2005; Sabra et al. 2005a).”
Traveltime measurements from noise correlation: stability and detection of instrumental time-shifts (2007, background): “This means than in average, between 1999 and 2005, more energy propagates from PAS to GSC than from GSC to PAS (Van Tiggelen 2003; Paul et al. 2005; Pedersen et al. 2006; Stehly et al. 2006).”
Lunar subsurface investigated from correlation of seismic noise (2005, background): “Though the pulse arrival times are symmetric, waveform amplitudes may change due to preferential direction of propagation of the incident wave field [van Tiggelen, 2003; Paul et al., 2005].”
Processing seismic ambient noise data to obtain reliable broad-band surface wave dispersion measurements (2007, methodology): “…based 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…”
Tomography of the Alpine region from observations of seismic ambient noise (2009, methodology): “In seismology this idea has been successfully applied to the seismic coda (Campillo & Paul 2003; Paul et al. 2005) and seismic noise (Shapiro & Campillo 2004; Shapiro et al. 2005; Sabra et al. 2005a).”
Retrieval of the Green’s Function from Cross Correlation: The Canonical Elastic Problem (2006, background): “The energy ratio stabilization appears before the complete isotropy of the field but indicates that the diffusion can be used as a good approximation (Paul et al., 2005).”
Characteristics of ambient seismic noise as a source for surface wave tomography (2008, background): “The first is seismic coda, which results from the multiple scattering of seismic waves by small-scale inhomogeneities [e.g., Aki and Chouet, 1975; Paul et al., 2005].”
A study of the seismic noise from its long-range correlation properties (2006, background): “In the case of diffuse coda waves, the averaging is performed over a set of earthquakes [Campillo and Paul, 2003; Paul et al., 2005].”