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      Characteristics of ambient seismic noise as a source for surface wave tomography : CHARACTERISTICS OF AMBIENT SEISMIC NOISE

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      Geochemistry, Geophysics, Geosystems
      American Geophysical Union (AGU)

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          High-Resolution Surface-Wave Tomography from Ambient Seismic Noise

          Cross-correlation of 1 month of ambient seismic noise recorded at USArray stations in California yields hundreds of short-period surface-wave group-speed measurements on interstation paths. We used these measurements to construct tomographic images of the principal geological units of California, with low-speed anomalies corresponding to the main sedimentary basins and high-speed anomalies corresponding to the igneous cores of the major mountain ranges. This method can improve the resolution and fidelity of crustal images obtained from surface-wave analyses.
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            Processing seismic ambient noise data to obtain reliable broad-band surface wave dispersion measurements

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              Origin of coda waves: Source, attenuation, and scattering effects

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                Author and article information

                Journal
                Geochemistry, Geophysics, Geosystems
                Geochem. Geophys. Geosyst.
                American Geophysical Union (AGU)
                15252027
                February 2008
                February 2008
                : 9
                : 2
                : n/a
                Article
                10.1029/2007GC001814
                7acba7c6-356c-4816-80ad-d5518271828a
                © 2008

                http://doi.wiley.com/10.1002/tdm_license_1.1

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