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- W2070651063 abstract "[1] An 18 a long experiment to capture changes in electrical resistivity prior to, during, and after a M6 earthquake on the San Andreas fault at Parkfield, California, culminated with an event of that magnitude on 28 September 2004. Resistivity was monitored with a telluric array, giving precisions in measured parameters of 0.2% or less. No coseismic resistivity changes greater than 5% could have occurred or they would have been detected by the array, and any precursory changes would have been much smaller because maximum possible precursory strains were 4000 times smaller than the coseismic strain. Given that the earthquake ruptured directly beneath the telluric array, this experiment places a bound on the amount resistivity might change at the hypocentral location; changes measured with instruments farther from earthquakes can only be smaller. It is still possible that a measurable change with a larger earthquake or other fault geometries are capable of generating larger signals, but our results show clearly that future experiments should be designed with precisions of much better than 0.1% if they are to be successful." @default.
- W2070651063 created "2016-06-24" @default.
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- W2070651063 date "2007-12-15" @default.
- W2070651063 modified "2023-09-27" @default.
- W2070651063 title "Electrical resistivity changes not observed with the 28 September 2004M6.0 Parkfield earthquake on the San Andreas fault, California" @default.
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- W2070651063 doi "https://doi.org/10.1029/2006jb004459" @default.
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