SOURCE PARAMETERS OF THE BORREGO MOUNTAIN EARTHQUAKE1 By MAx WYss
نویسندگان
چکیده
Spectral analysis of teleseismic body phases at several azimuths was used to determine the moment, fault length, dislocation, stress-drop, and radiated energy of the Borrego Mountain earthquake. The results agree well with the same parameters obtained from the surface fracture and aftershock distribution and local observations of radiated energy.
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