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U.S. GEOLOGICAL SURVEY, 345 MIDDLEFIELD ROAD, MENLO PARK, CALIFORNIA 94025
Abstract
Two geodetic stations, the positions of which are frequently monitored by geodetic distance-measuring techniques, were located 5 and 10 km from the epicentral area of the Briones Hills earthquake swarm (maximum magnitude ML = 4.3) of January 1977. Although a 10 µradian postearthquake tilt change was recorded at a nearby tiltmeter, no significant change in geodetic distances could be detected at a sensitivity of at least 0.5 ppm. A simple dislocation model of the main earthquake in the swarm would predict no observable change in either tilt or geodetic distance.
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M. J. S. JOHNSTON, A. C. JONES, W. DAUL, and C. E. MORTENSEN Tilt near an earthquake (ML = 4.3), Briones Hills, California Bulletin of the Seismological Society of America, February 1, 1978; 68(1): 169 - 173. [Abstract] [PDF] |
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