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- W2066528026 abstract "By using seismic records of the 2004 magnitude 6.0 Parkfield earthquake, we identified a burst of high-frequency seismic radiation that occurred about 13 kilometers northwest of the hypocenter and 5 seconds after rupture initiation. We imaged this event in three dimensions by using a waveform back-projection method, as well as by timing distinct arrivals visible on many of the seismograms. The high-frequency event is located near the south edge of a large slip patch seen in most seismic and geodetic inversions, indicating that slip may have grown abruptly at this point. The time history obtained from full-waveform back projection suggests a rupture velocity of 2.5 kilometers per second. Energy estimates for the subevent, together with long-period slip inversions, indicate a lower average stress drop for the northern part of the Parkfield earthquake compared with that for the region near its hypocenter, which is in agreement with stress-drop estimates obtained from small-magnitude aftershocks." @default.
- W2066528026 created "2016-06-24" @default.
- W2066528026 creator A5014518055 @default.
- W2066528026 creator A5076510143 @default.
- W2066528026 date "2007-11-23" @default.
- W2066528026 modified "2023-10-10" @default.
- W2066528026 title "A High-Frequency Secondary Event During the 2004 Parkfield Earthquake" @default.
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- W2066528026 doi "https://doi.org/10.1126/science.1146537" @default.
- W2066528026 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/18033878" @default.
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