Imaging from one-bit correlations of wideband diffuse wave fields

By É. Larose, A. Derode, Michel Campillo, Mathias Fink. 2004

198 citations recorded by the source corpus.

Subfields: Geophysics, Mechanics of Materials

View Paper: https://www.semanticscholar.org/paper/80bba60cea34d65bee95fff645b55e157d40eb1c

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In Mechanics of Materials

Citations in the corpus

Extracting time‐domain Green's function estimates from ambient seismic noise (2005, methodology): “Experimental evidence of this result has been presented in helioseismology [Rickett and Claerbout ,1 999], ultrasonics [Lobkis and Weaver, 2001; Weaver and Lobkis, 2003; Larose et al., 2004; Malcolm et al., 2004; Weaver and Lobkis, 2004], underwater acoustics [Roux et al., 2004; Sabra et al., 2005”
Imaging preeruptive and coeruptive structural and mechanical changes of a volcano with ambient seismic noise (2013, methodology): “We apply 1 bit amplitude normalization [Larose et al., 2004] and cross-correlate the vertical component of the seismic noise between all of the stations.”
Broadband ambient noise surface wave tomography across the United States (2008, background): “Initially, researchers favored a 1-bit (or sign bit, or binary) normalization [Larose et al., 2004; Shapiro et al., 2005], but Bensen et al. [2007] argued for the application of a temporally variable weighting function to retain more of the small amplitude character of the raw data and to allow for…”
Empirical synthesis of time-asymmetrical Green functions from the correlation of coda waves (2005, background): “[10] Derode et al. [2003b] and Larose et al. [2004] showed the role of multiple scattering in enhancing the efficiency of the reconstruction of the Green function with a limited number of sources and finite durations of recording, in conditions closer to seismology.”
Reconstructing Green's function by correlation of the coda of the correlation (C3) of ambient seismic noise (2008, methodology): “The convergence toward the Green’s function, i.e., the ratio of amplitude of R over residual fluctuations, is evolving as the square root of the amount of data used in the cross correlation [Larose et al., 2004; Snieder, 2004; Sabra et al., 2005a; Weaver and Lobkis, 2005].”
Ambient noise Rayleigh wave tomography across Europe (2007, methodology): “For this purpose, Shapiro et al. (2005) used one-bit normalization, which generates a data stream composed only of the values 1 and −1, retaining only the sign and disregarding the amplitude of the signal completely (Larose et al. 2004).”
Spurious multiples in seismic interferometry of primaries (2006, methodology): “The reconstruction of the Green’s function from recordings of incoherent signals has been shown observationally using ultrasound [Weaver and Lbkis, 2001; Larose et al., 2004; Malcolm et al., 2004].”
Processing seismic ambient noise data to obtain reliable broad-band surface wave dispersion measurements (2007, methodology): “This method has been shown to increase signal-to-noise ratio (SNR) when employed in acoustic experiments in the laboratory (Larose et al. 2004) and has been used in a number of early seismic studies of coda waves and ambient noise (Campillo & Paul 2003; Shapiro & Campillo 2004; Shapiro et al. 2005;…”