Bulletin of the Seismological Society of America
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Bulletin of the Seismological Society of America; June 1983; v. 73; no. 3; p. 735-748
© 1983 Seismological Society of America
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by BOLT, B. A.
Right arrow Articles by HERRAIZ, M.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Simplified estimation of seismic moment from seismograms

BRUCE A. BOLT and MIGUEL HERRAIZ

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


Formula

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, {Delta} 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


Formula

where Mo is dyne-cm, C in millimeters, D in seconds, and {Delta} in kilometers.

The corresponding moment-magnitude relation is


Formula

for 3 less double equals ML less double equals 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 less double equals ML less double equals 5.1).




This article has been cited by other articles:


Home page
Bulletin of the Seismological Society of AmericaHome page
W. J. Person
Seismological notes--November-December 1993
Bulletin of the Seismological Society of America, October 1, 1994; 84(5): 1687 - 1700.
[PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
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]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 1983 by the Seismological Society of America.