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Article |
United States Geological Survey
Pasadena,
Californi
(S.E.H.)
I use seismic data from portable digital stations and the broadband
Terrascope network in southern California to investigate radiated earthquake
source spectra and discuss the results in light of previous studies on both
static stress drop and apparent stress. Applying the empirical Green's
function (EGF) method to two sets of M 46.1 events, I obtain
deconvolved source-spectra estimates and corner frequencies. The results are
consistent with an
2 source model and constant Brune stress
drop. However, consideration of the raw spectral shapes of the largest events
provides evidence for a high-frequency decay more shallow than
2. The intermediate (
f1)
slope cannot be explained plausibly with attenuation or site effects and is
qualitatively consistent with a model incorporating directivity effects and a
fractional stress-drop rupture process, as suggested by Haddon
(1996). However, the results
obtained in this study are not consistent with the model of Haddon
(1996) in that the
intermediate slope is not revealed with EGF analysis. This could reflect
either bandwidth limitations inherent in EGF analysis or perhaps a rupture
process that is not self-similar. I show that a model with an intermediate
spectral decay can also reconcile the apparent discrepancy between the scaling
of static stress drop and that of apparent stress drop for moderate-to-large
events.
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