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Detection of Crustal Deformation from the Landers Earthquake Sequence using Continuous Geodetic Measurements

Yehuda Bock, Duncan C. Agnew, Peng Fang, Joachim F. Genrich, Bradford H. Hager, Thomas A. Herring, Kenneth W. Hudnut, Robert W. King, Shawn Larsen, Jean B. Minster, Keith F. Stark, & Frank K. Wyatt

Published 1993, SCEC Contribution #8

THE measurement of crustal motions in technically active regions is being performed increasingly by the satellite-based Global Positioning System (GPS)1,2, which offers considerable advantages over conventional geodetic techniques3,4. Continuously operating GPS arrays with ground-based receivers spaced tens of kilometres apart have been established in central Japan5,6 and southern California to monitor the spatial and temporal details of crustal deformation. Here we report the first measurements for a major earthquake by a continuously operating GPS network, the Permanent GPS Geodetic Array (PGGA)7–9 in southern California. The Landers (magnitude Afw of 7.3) and Big Bear (M w 6.2) earthquakes of 28 June 1992 were monitored by daily observations. Ten weeks of measurements, centred on the earthquake events, indicate significant coseismic motion at all PGGA sites, significant post-seismic motion at one site for two weeks after the earthquakes, and no significant preseismic motion. These measurements demonstrate the potential of GPS monitoring for precise detection of precursory and aftershock seismic deformation in the near and far field.

Bock, Y., Agnew, D. C., Fang, P., Genrich, J. F., Hager, B. H., Herring, T. A., Hudnut, K. W., King, R. W., Larsen, S., Minster, J. B., Stark, K. F., & Wyatt, F. K. (1993). Detection of Crustal Deformation from the Landers Earthquake Sequence using Continuous Geodetic Measurements. Nature, 361(6410), 337-340. doi: 10.1038/361337a0.