Published May 1983
| Published
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Mechanism of the 1983 Coalinga earthquake determined from long-period surface waves
- Creators
-
Kanamori, Hiroo
- Others:
- Bennett, John H.
- Sherburne, Roger W.
Chicago
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Abstract
The mechanism of the May 2, 1983, Coalinga, California earthquake determined from long-period surface waves and first-motion data is given by dip angle = 65º, strike = N58°W, rake = 70°, seismic moment = 5.4 x 10^(25) dyne-cm (M_w = 6.4), and the source process time ≃ 20 sec. The local magnitude, M_L, is estimated to be 6.43 ± 0.27. On the M_L vs. M_w diagram, the Coalinga earthquake falls on the average trend for California earthquakes.
Additional Information
© 1983 American Geosciences Institute. Special Publication - California Department of Conservation, Division of Mines and Geology.Attached Files
Published - HKcdmg83.pdf
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Additional details
- Eprint ID
- 54838
- Resolver ID
- CaltechAUTHORS:20150213-134715035
- Created
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2015-02-17Created from EPrint's datestamp field
- Updated
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2020-03-09Created from EPrint's last_modified field
- Caltech groups
- Division of Geological and Planetary Sciences (GPS)
- Series Name
- Special publication (California Division of Mines and Geology)
- Series Volume or Issue Number
- 66