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MARINE SCIENCE INSTITUTE AND DEPARTMENT OF GEOLOGICAL SCIENCES UNIVERSITY OF CALIFORNIA, SANTA BARBARA, CALIFORNIA 93106
Abstract
Anomalous drift of a theodolite plate-level bubble was observed about 5 hr before two of the stronger aftershocks of the San Fernando earthquake of February 9, 1971. The phenomenon may be related to crustal tilting during the accumulation of strain prior to the aftershocks.
This article has been cited by other articles:
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T. RIKITAKE Earthquake precursors Bulletin of the Seismological Society of America, October 1, 1975; 65(5): 1133 - 1162. [Abstract] [PDF] |
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