Surface wave tomography from microseisms in Southern California

  • Karim G. Sabra
    Marine Physical Laboratory of the Scripps Institution of Oceanography University of California San Diego, La Jolla California USA
  • Peter Gerstoft
    Marine Physical Laboratory of the Scripps Institution of Oceanography University of California San Diego, La Jolla California USA
  • Philippe Roux
    Marine Physical Laboratory of the Scripps Institution of Oceanography University of California San Diego, La Jolla California USA
  • W. A. Kuperman
    Marine Physical Laboratory of the Scripps Institution of Oceanography University of California San Diego, La Jolla California USA
  • Michael C. Fehler
    Los Alamos National Laboratory Los Alamos New Mexico USA

書誌事項

公開日
2005-07-26
権利情報
  • http://onlinelibrary.wiley.com/termsAndConditions#vor
DOI
  • 10.1029/2005gl023155
公開者
American Geophysical Union (AGU)

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説明

<jats:p>Since it has already been demonstrated that point‐to‐point seismic propagation Green Functions can be extracted from seismic noise, it should be possible to image Earth structure using the ambient noise field. Seismic noise data from 148 broadband seismic stations in Southern California were used to extract the surface wave arrival‐times between all station pairs in the network. The seismic data were then used in a simple, but densely sampled tomographic procedure to estimate the surface wave velocity structure within the frequency range of 0.1–0.2 Hz for a region in Southern California. The result compares favorably with previous estimates obtained using more conventional and elaborate inversion procedures. This demonstrates that coherent noise field between station pairs can be used for seismic imaging purposes.</jats:p>

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