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SEISMOGRAPHIC STATION UNIVERSITY OF CALIFORNIA, BERKELEY, CALIFORNIA 94720
CÁTEDRA DE GEOFÍSICA FACULTAD DE CIENCIAS FÍSICAS UNIVERSIDAD COMPLUTENSE, MADRID3, Spain
Abstract
This study proposes a method to estimate the seismic moment of regional and local earthquakes based on simple measurements made directly on Wood-Anderson seismograms. The method parallels the routine estimation of local magnitude in observatory work. The relation used is
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where C is the maximum peak-to-peak amplitude read on a Wood-Anderson seismogram, D is the duration between the S arrival and the onset with amplitude C/d,
is epicentral distance, and a, b, p, and d are constants. The form of the logarithmic term is suggested by the analytical expression for moment (Keilis-Borok, 1960).
Least-squares fits were made to data from 73 Wood-Anderson records of 16 central California earthquakes with seismic moments already evaluated independently from spectral analysis or broadband displacement records. The values p = 1, d, = 3 proved appropriate and subsequent regression yielded
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where Mo is dyne-cm, C in millimeters, D in seconds, and
in kilometers.
The corresponding moment-magnitude relation is
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for 3
ML
6.2.
The latter fit is close to an earlier empirical result (Johnson and McEvilly, 1974) for central California based on fewer cases and a different range of magnitude (2.4
ML
5.1).
This article has been cited by other articles:
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W. J. Person Seismological notes--November-December 1993 Bulletin of the Seismological Society of America, October 1, 1994; 84(5): 1687 - 1700. [PDF] |
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R. A. UHRHAMMER and B. A. BOLT The seismic magnitude of the 1989 Loma Prieta mainshock determined from strong motion records Bulletin of the Seismological Society of America, October 1, 1991; 81(5): 1511 - 1517. [Abstract] [PDF] |
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