Bulletin of the Seismological Society of America; December 2003; v. 93; no. 6;
p. 2415-2433; DOI: 10.1785/0120020226
© Seismological Society of America
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Figure 9. Long-term creep rate shown versus distance from the MTJ as described in Figure 8. Solid numbered triangles are arrays in this study; inverted solid triangles are arrays of Burford and Harsh (1980); open triangle A, span of Sleepy-San Pablo line; circles B through K, geodetic data referenced in caption of Figure 8. For the Hayward fault the mean ±2
lines show uncertainty range of best-fit polynomials that express the along-strike variation in long-term creep rate derived from the much larger data set for this fault (Lienkaemper et al., 2001). Data for sites 24 and 27 reflect pre-LPEQ rates of Lienkaemper and Galehouse (1997) and Harsh and Burford (1982). Dashed lines are interpolated between available data; queries indicate areas where major gaps in the data exist. For the Paicines-San Benito section of the Calaveras subsystem, two dashed lines illustrate possible alternative interpretations of existing data.
