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Seismic interferometry: Who needs a seismic source?. Roel Snieder Center for Wave Phenomena Colorado School of Mines email rsnieder@mines.edu http://www.mines.edu/~rsnieder download publications from: http://www.mines.edu/~rsnieder/Publications.html. F. (Einstein, 1905).
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Seismic interferometry:Who needs a seismic source? Roel Snieder Center for Wave Phenomena Colorado School of Mines email rsnieder@mines.edu http://www.mines.edu/~rsnieder download publications from: http://www.mines.edu/~rsnieder/Publications.html
F (Einstein, 1905) Fluctuation-dissipation theorem (Kubo, Rep. Prog. Phys., 29, 255-284, 1966)
Very Long Baseline Interferometry http://www.lupus.gsfc.nasa.gov/brochure/bintro.html
Distance between USA and Germany http://www.lupus.gsfc.nasa.gov/brochure/btoday2.html
Pseudo-random source Piezo-electric vibrator from CGG
Coda wave interferometry 45°C 50°C (Snieder et al., Science, 295, 2253-2255, 2002)
Cross-correlation • sum of causal and acausal response • uncorrelated left- and rightgoing waves
Need to extend this to include: • heterogeneous media • - more space dimensions
Derivation based on normal-modes (Lobkis and Weaver, JASA, 110, 3011-3017, 2001)
Displacement response Heaviside function
Correlation Green’s function
Correlation Green’s function
Correlation Green’s function
Correlation and Green’s function • sum of causal and acausal Green’s function • holds for arbitrary heterogeneity
Dealing with with acausal Green’s function • truncate correlation for t<0 • average correlation for t<0 and t>0
Displacement instead of velocity Conclusion: time derivative may appear
Acoustic waves Green’s function:
Time reversal = complex conjugation Time-reversed solution
Time-reversal When is a solution. then is a solution as well N.B. this does not hold in the presence of attenuation
Representation theorem replace:
Left hand side reciprocity
For spherical surface far away Radiation condition:
Virtual-sources (Wapenaar, Fokkema, and Snieder, JASA, 118, 2783-2786 2005 heuristic derivation: Derode et al., JASA, 113, 2973-2976, 2003)
Computing synthetic seismograms (Van Manen et al., Phys. Rev. Lett., 94, 164301,2005)
Field example of virtual sources complicated overburden reservoir (Bakulin and Calvert, SEG expanded abstracts, 2477-2480, 2004)
Peace River 4D VSP Component used, along-the-well (450)
Image from virtual sources top bottom
Virtual source Surface
Virtual-sources (Wapenaar, Fokkema, and Snieder, JASA, 118, 2783-2786 2005 heuristic derivation: Derode et al., JASA, 113, 2973-2976, 2003)
Excitation by uncorrelated sources on surface • Uncorrelated sources can be: • sequential shots • uncorrelated noise
Green’s function from uncorrelated sources (For elastic waves: Wapenaar, Phys. Rev. Lett, 93, 254301, 2004)
Raindrop model • Sources can be: • real sources • secondary sources (scatterers)