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A local earthquake coda magnitude and its relation to duration, moment M_o, and local Richter magnitude M_L

Suteau, Anne M. and Whitcomb, James H. (1979) A local earthquake coda magnitude and its relation to duration, moment M_o, and local Richter magnitude M_L. Bulletin of the Seismological Society of America, 69 (2). pp. 353-368. ISSN 0037-1106. http://resolver.caltech.edu/CaltechAUTHORS:20140812-143740373

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Abstract

A relationship is found between the seismic moment, M_o, of shallow local earthquakes, coda amplitudes, and the total duration of the signal, t, in seconds, measured from the earthquake origin time. Following Aki, we assume that the end of the coda is composed of backscattering surface waves due to lateral heterogeneity in the shallow crust. Using the linear relationship between the logarithm of M_o and the local Richter magnitude M_L, we obtain a relationship between M_L and t, of the form: M_L = a_0 + a_1 log t + a_2t^(1/3) + f(t), where a_0, a_1, a_2 are constants depending on an attenuation parameter (effective Q) and geometric spreading; and f(t) is a function of the instrument response and a (weak) function of the scattering process. This relationship is different from the empirical one generally used M_L = a_0 + a_1 log τ + a_2(log τ)^2 + a_3Δ, where τ is the duration measured from the first P arrival time and Δ is epicentral distance in kilometers. In the theoretical relationship, the dependence on epicentral distance is implicit in t. The theoretical relationship is used to calculate a coda magnitude M_C that is compared to M_L for southern California earthquakes which occurred during the period from 1972 to 1975. This comparison is made independently at six stations of the CIT network. At all stations, a good linear fit (M_L = C_0 + C_1M_C) is obtained. The standard errors range from 0.2 to 0.3 and the correlation coefficients from 0.80 to 0.90. Once station gain is accounted for, station correction terms are less than 0.17 magnitude unit when comparing M_L and M_c. M_c calculation is not limited to a duration measurement but can utilize the entire earthquake coda in order to increase by many times the statistical confidence in an estimate of an earthquake's magnitude.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://bssa.geoscienceworld.org/content/69/2/353.abstractPublisherArticle
Alternate Title:A local earthquake coda magnitude and its relation to duration, moment Mo, and local Richter magnitude ML
Additional Information:Copyright © 1979, by the Seismological Society of America. Manuscript received July 28, 1978. The authors wish to thank Don Anderson, Keiiti Aki, William Bakun, Carl Johnson, Karen McNally, and Bernard Minster for critically reviewing the manuscript and providing several helpful suggestions. The data used in this paper is due to many individuals at the Seismological Laboratory who maintain the network and process the data and their efforts are greatly appreciated. This work was supported by JPL/NASA Contract 49-681-02081-0-3260, NASA Grant NSG-5224, and U.S.G.S. Contract 14-08-0001-16719.
Funders:
Funding AgencyGrant Number
JPL/NASA49-681-02081-0-3260
NASANSG-5224
USGS14-08-0001-16719
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Caltech Division of Geological and Planetary Sciences3062
Record Number:CaltechAUTHORS:20140812-143740373
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20140812-143740373
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:48434
Collection:CaltechAUTHORS
Deposited By: George Porter
Deposited On:12 Aug 2014 22:35
Last Modified:13 Feb 2019 18:06

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