Retrieving the Green’s function in an open system by cross correlation : A comparison of approaches (L)

By Kees Wapenaar, Jacob T. Fokkema, Roel Snieder. 2005

177 citations recorded by the source corpus.

Subfields: Geophysics, Ocean Engineering

View Paper: https://www.semanticscholar.org/paper/be91b730451d8561b1ce23dabc1e876beae49e24

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Geophysics

1. Roel Snieder
2. Kees Wapenaar
3. Evert C. Slob
4. J. Neut
5. Andrew Curtis
6. K. Larner
7. Kurang Mehta
8. V. Graizer

In Ocean Engineering

1. Kees Wapenaar
2. Roel Snieder
3. J. Neut
4. Kurang Mehta
5. V. Graizer
6. Andrew Curtis
7. K. Larner
8. Evert C. Slob

Citations in the corpus

• Extraction of near-surface properties for a lossy layered medium using the propagator matrix (2007, methodology): “…Derode et al. 2003; Kawakami & Oyunchimeg 2003; Schuster et al. 2004; Shapiro & Campillo 2004; Snieder 2004; Wapenaar 2004; Shapiro et al. 2005; Wapenaar et al. 2005; Snieder et al. 2006a) is a technique based on combining signals recorded at different sensors, to estimate the response between…”
• Seismic interferometry by crosscorrelation and by multidimensional deconvolution: a systematic comparison (2010, background): “Assuming the medium in V is lossless, the correlation-type representation for the acoustic Green's function between xA and xB in V reads (Wapenaar et al. 2005; van Manen et al. 2005) ˆ ¯ G(xB, xA, ω) + ˆ G * (xB, xA, ω) = (1) − S 1 jωρ(x) ∂î ¯ G(xB, x, ω) ˆ G * (xA, x, ω) − ˆ ¯ G(xB, x, ω)∂î G *…”
• Spurious multiples in seismic interferometry of primaries (2006, background): “This is a puzzling conclusion, since theory predicts that the full Green’s function can be retrieved when the sources are placed on a closed surface that surrounds the region of interest [Wapenaar et al., 2004; Wapenaar et al., 2005].”
• Connection of scattering principles: a visual and mathematical tour (2012, unknown): “…a technique that allows one to reconstruct the response between two receivers (represented by the two triangles at locations RA and RB in figure 2) from the cross-correlation of the wavefield measured at these two receivers which are excited by uncorrelated sources surrounding the studied system.”
• Tutorial on seismic interferometry: Part 2 — Underlying theory and new advances (2010, background): “…1988; Fokkema and van den Berg, 1993 and the principle of time-reversal invariance Bojarski, 1983; Fink, 1992 , we obtain the acoustic analogue of equation 8 according to Ĝ xB,xA, Ĝ* xB,xA, D 1 j x iĜ xB,x, Ĝ* xA,x, Ĝ xB,x, iĜ* xA,x, nid2x 11 van Manen et al., 2005; Wapenaar et al., 2005 .”
• Focusing the wavefield inside an unknown 1D medium: Beyond seismic interferometry (2012, methodology): “This technique allows one to reconstruct the wavefield that propagates between a virtual source and other receivers located inside the medium (Wapenaar et al., 2005).”