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Title: Combined inversion for the three-dimensional Q structure and source parameters using microearthquake spectra

Journal Article · · Journal of Geophysical Research; (United States)
OSTI ID:5014136
 [1]
  1. Univ. of Colorado, Boulder (United States)

The estimation of Q values and/or source corner frequencies f{sub c} from single-station narrow-band recordings of microearthquake spectra is a strongly nonunique problem. This is due to the fact that the spectra can be equally well fitted with low-Q/high-f{sub c} or a high-Q/low f{sub c} spectral models. Here, a method is proposed to constrain this ambiguity by inverting a set of microearthquake spectra for a three-dimensional Q model structure and model source parameters seismic moment (M{sub o}) and corner frequency (f{sub c}) simultaneously. The inversion of whole path Q can be stated as a linear problem in the attenuation operator l* and solved using a tomographic reconstruction of the three-dimensional Q structure. This Q structure is then used as a geometrical constraint for a nonlinear Marquardt-Levenberg inversion of M{sub o} and f{sub c} and a new Q value. The method has been tested on a set of approximately 2,800 P wave spectra from the recordings of 635 microearthquakes from the Kaoiki seismic zone in Hawaii which were recorded at up to six stations. The hypocenters are distributed within a volume of approximately 18 {times} 18 {times} 15 km (depth). The Q model uncertainties have been estimated on the basis of several different tests: Self-consistency, constraining the corner frequencies, and additionally splitting the data set. The standard deviation of the final Q model which used a grid size of 1.5 {times} 1.5 {times} 2.0 km (depth) was less than 3% for the depth range 0-5 km, less than 5% between 5 and 7 km, and 7% between 7 and 9 km. For the given data set and depths below 3-5 km, the method is believed to be able to resolve the model dependent attenuation structure on a scale down to 1-2 km with a resolution of a few percent.

OSTI ID:
5014136
Journal Information:
Journal of Geophysical Research; (United States), Vol. 95:B8; ISSN 0148-0227
Country of Publication:
United States
Language:
English