Southern California Permanent GPS Geodetic Array: Continuous measurements of regional crustal deformation between the 1992 Landers and 1994 Northridge earthquakes

Yehuda Bock, Shimon Wdowinski, Peng Fang, Jie Zhang, Stanley Williams, H Johnson, Jeff Behr, Joachim F. Genrich, Jeffrey Dean, Matt van Domselaar, Duncan C. Agnew, Frank K. Wyatt, Keith F. Stark, B Oral, Kenneth W. Hudnut, Robert W. King, Thomas A. Herring, S Dinardo, William Young, David D. Jackson, & Werner Gurtner

Published 1997, SCEC Contribution #328b

The southern California Permanent GPS Geodetic Array (PGGA) was established in 1990 across the Pacific-North America plate boundary to continuously monitor crustal deformation. We describe the development of the array and the time series of daily positions estimated for its first 10 sites in the 19-month period between the June 28, 1992 (M w =7.3), Landers and January 17, 1994 (M w =6.7), Northridge earthquakes. We compare displacement rates at four site locations with those reported by Feigl et al. [1993], which were derived from an independent set of Global Positioning System (GPS) and very long baseline interferometry (VLBI) measurements collected over nearly a decade prior to the Landers earthquake. The velocity differences for three sites 65–100 km from the earthquake's epicenter are of order of 3–5 mm/yr and are systematically coupled with the corresponding directions of coseismic displacement. The fourth site, 300 km from the epicenter, shows no significant velocity difference. These observations suggest large-scale postseismic deformation with a relaxation time of at least 800 days. The statistical significance of our observations is complicated by our incomplete knowledge of the noise properties of the two data sets; two possible noise models fit the PGGA data equally well as described in the companion paper by Zhang et al. [this issue]; the pre-Landers data are too sparse and heterogeneous to derive a reliable noise model. Under a fractal white noise model for the PGGA data we find that the velocity differences for all three sites are statistically different at the 99% significance level. A white noise plus flicker noise model results in significance levels of only 94%, 43%, and 88%. Additional investigations of the pre-Landers data, and analysis of longer spans of PGGA data, could have an important effect on the significance of these results and will be addressed in future work.

Citation
Bock, Y., Wdowinski, S., Fang, P., Zhang, J., Williams, S., Johnson, H., Behr, J., Genrich, J. F., Dean, J., van Domselaar, M., Agnew, D. C., Wyatt, F. K., Stark, K. F., Oral, B., Hudnut, K. W., King, R. W., Herring, T. A., Dinardo, S., Young, W., Jackson, D. D., & Gurtner, W. (1997). Southern California Permanent GPS Geodetic Array: Continuous measurements of regional crustal deformation between the 1992 Landers and 1994 Northridge earthquakes. Journal of Geophysical Research, 102(B8), 55-61. doi: 10.1029/97JB01379.