Source parameters of the June 29, 1992 Little Skull Mountain Earthquake from complete regional waveforms at a single station

The June 29, 1992, m{sub b} = 5.5, Little Skull Mountain earthquake occurred 20 km southeast of Yucca Mountain within the boundaries of the Nevada Test Site. This event was recorded at a very broadband station located about 310 km to the east at Kanab, Utah. Both body and surface waves from this single station were used in a grid search technique for the best fitting double couple moment tensor. The technique minimizes the misfit between reflectivity generated complete synthetic seismograms and the three-component displacement data via a search over the strike, dip and rake of the source. In the passband of 50-15 s period, the grid search results in a well defined, nearly pure normal mechanism with a strike of 35{degrees}, a dip of 54{degrees}, a rake of {minus}87{degrees}, and a seismic moment of 4.1 x 10{sup 17} N-m. Applying the same technique to the large aftershock on July 5, 1992 the authors obtain a somewhat less well defined minimum with a strike of 358{degrees}, a dip of 36{degrees}, a rake of {minus}177{degrees}, and a moment of 4.3 x 10{sup 15} N-m. The minimum-compression axes of these mechanisms are consistent with northwest-southeast extension in the Basin and Range. 14more » refs., 7 figs.« less

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