Bulletin of the Seismological Society of America; February 2006; v. 96; no. 1;
p. 11-32; DOI: 10.1785/0120040166
© Seismological Society of America
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Figure 6. The magnitude of the velocity field determined from inversion of geodetic
data (see text) as a function of XSW, the perpendicular
distance from the southwestern boundary of the study region. The profiles are
located along the upper half of domain A and the centers of domains B, C, and D
(Fig. 5). Modeled velocities
are shown (solid circles) along with one-standard-deviation error bars.
GPS data used to derive the model are also shown (open circles) as
well as their one-standard-deviation uncertainty limits.
