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Allmann BP, Shearer PM. A high-frequency secondary event during the 2004 Parkfield earthquake. Science. 2007;318(5854):1279-83doi: 10.1126/science.1146537.
Allmann, B. P., & Shearer, P. M. (2007). A high-frequency secondary event during the 2004 Parkfield earthquake. Science (New York, N.Y.), 318(5854), 1279-83. https://doi.org/10.1126/science.1146537
Allmann, Bettina P, and Shearer, Peter M. "A high-frequency secondary event during the 2004 Parkfield earthquake." Science (New York, N.Y.) vol. 318,5854 (2007): 1279-83. doi: https://doi.org/10.1126/science.1146537
Allmann BP, Shearer PM. A high-frequency secondary event during the 2004 Parkfield earthquake. Science. 2007 Nov 23;318(5854):1279-83. doi: 10.1126/science.1146537. PMID: 18033878.
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Science. 2007 Nov 23;318(5854):1279-83. doi: 10.1126/science.1146537.

A high-frequency secondary event during the 2004 Parkfield earthquake.

Science (New York, N.Y.)

Bettina P Allmann, Peter M Shearer

Affiliations

  1. Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California San Diego, 9500 Gilman Drive, La Jolla, CA 92093-0225, USA. [email protected]

PMID: 18033878 DOI: 10.1126/science.1146537

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.

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