Bulletin of the Seismological Society of America; February 2006; v. 96; no. 1;
p. 288-305; DOI: 10.1785/0120040102
© Seismological Society of America
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Figure 6. An along-strike cross-sectional view of hypocenters in the central segment of
the NMSZ (BB' in
Figs. 2–4) showing that
the preliminary earthquake locations using the PANDA model (crosses)
are very similar to those relocated using the newly developed
single-event-location program with the available 3D VP and
VS models (open circles). The thickness of the sediments in
this region is very close to that in the PANDA model. Seismicity in
the central NMSZ is the highest in the region, and it is impossible
to visualize the differences in hypocenters before and after the relocation if
all earthquakes are shown in the same cross-section. Therefore, only randomly
selected earthquakes are displayed in this cross-section. The vertical and
horizontal scales are equal.
