|Title||An improved method to determine coda-Q, earthquake magnitude, and site amplification: Theory and application to Southern California|
|Publication Type||Journal Article|
|Year of Publication||2019|
|Authors||Wang W., Shearer PM|
|Journal||Journal of Geophysical Research-Solid Earth|
|Type of Article||Article|
|Keywords||duration magnitudes; Geochemistry & Geophysics; intrinsic absorption; lapse-time dependence; local earthquakes; radiative-transfer; s-wave coda; scattering attenuation; shear-waves; spatial-distribution; temporal stability|
Seismic coda waves can be used to constrain attenuation, estimate earthquake magnitudes, and determine site amplification factors. We have developed a new multistation and multievent method to determine these three important seismic parameters simultaneously. We analyze 642 representative local (100 km) and shallow (20 km) earthquakes with catalog magnitudes between 1.8 and 5.4 in southern California at multiple frequency bands centered at 1.5, 3, 6, and 12 Hz. We find that the length of the moving average time window can affect the measurement of coda attenuation Q(C), but our tests indicate that the optimal window length is about 15 times the dominant data period. We use linear regression to fit each coda section and use only those portions that agree with the model decay rate with a correlation coefficient larger than 0.9. For a frequency-dependent coda-Q(C) model (Q(C) = Q(0)f(n)) at 1-Hz reference frequency, our results yield estimates for Q(0) and n of 107-288 and 0.42-1.14, respectively. Our coda magnitude estimates are linearly correlated with catalog magnitudes, and our observed lateral variations in coda-Q(C) and our site amplification factors are in general agreement with previous results, although there are notable differences at some locations. This approach provides a unified, accurate, and stable method to measure coda-Q(C), earthquake magnitude, and site amplification using coda waves of locally recorded earthquakes.