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Extracting the Green’s function from the correlation of coda waves: A derivation based on stationary phase

Physical Review E · 2004 · Vol. 69(4) · pp. 046610–046610
Roel Snieder

Abstract

The Green's function of waves that propagate between two receivers can be found by cross-correlating multiply scattered waves recorded at these receivers. This technique obviates the need for a source at one of these locations, and is therefore called "passive imaging." This principle has been explained by assuming that the normal modes of the system are uncorrelated and that all carry the same amount of energy (equipartitioning). Here I present an alternative derivation of passive imaging of the ballistic wave that is not based on normal modes. The derivation is valid for scalar waves in three dimensions, and for elastic surface waves. Passive imaging of the ballistic wave is based on the destructive interference of waves radiated from scatterers away from the receiver line, and the constructive interference of waves radiated from secondary sources near the receiver line. The derivation presented here shows that the global requirement of the equipartitioning of normal modes can be relaxed to the local requirement that the scattered waves propagate on average isotropically near the receivers.

Seismic Waves and AnalysisSeismic Imaging and Inversion TechniquesGeophysics and Sensor TechnologyPhysicsInterference (communication)CodaAcousticsRayleigh waveMechanical waveScalar (mathematics)Phase (matter)Love waveSurface wave

Funding

  • National Science Foundation
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References
On the emergence of the Green’s function in the correlations of a diffuse field
The Journal of the Acoustical Society of America · 2001 · 1,031 citations
Faster, Better: Shear-Wave Velocity to 100 Meters Depth from Refraction Microtremor Arrays
Bulletin of the Seismological Society of America · 2001 · 697 citations
A relational model of data for large shared data banks
Communications of the ACM · 1983 · 4,829 citations
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