Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2918
AuthorsMayeda, K.* 
Malagnini, L.* 
Walter, W.* 
TitleEvidence for departure in self-similarity: a new spectral ratio method using narrowband coda envelopes
Issue Date2007
Series/Report no./ 34 (2007)
DOI10.1029/2007GL030041
URIhttp://hdl.handle.net/2122/2918
Keywordsnon-self-similarity
Subject Classification04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamics 
AbstractThe use of local and regional S-wave coda is shown to provide stable amplitude ratios that better constrains source differences between event pairs. We first compared amplitude ratio performance between local and near regional S and coda waves in the San Francisco Bay region for moderate-sized events, then applied the coda spectral ratio method to the 1999 Hector Mine mainshock and its larger aftershocks. We find (1) average amplitude ratio standard deviations using coda are ~0.05 to 0.12, roughly a factor of 3 smaller than direct S-waves for 0.2 < f < 15.0 Hz; (2) coda spectral ratios for the Mw 7.0 Hector Mine earthquake and its aftershocks show a clear departure from self-similarity, consistent with other studies using the same datasets; and (3) event-pairs (Green’s function and target events) can be separated by ~25 km for coda amplitudes without any appreciable degradation, in sharp contrast to direct waves.
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