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We apply this method to the earthquake location problem.
For the modeling, the "earthquake location uncertainty" concept was employed.
To do this, accurate information regarding earthquake location is essential.
The first step that should be done on earthquake analysis is earthquake location determination.
An earthquake location includes a geographical position, a depth and an origin time.
To reduce uncertainty, we applied the double-difference earthquake location method (Waldhauser and Ellsworth, 2000).
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Figure 2 Earthquake locations and 1D velocity model.
Fig. 6 Vertical deformation and earthquake locations from the tensile crack model.
This feature is similar to the case of earthquake locations (Fig. 7).
Figure 3 Earthquake locations projected on the perspective view of the bathymetry and time-migrated sections.
On the cross-sections, the earthquake locations are plotted at 0.5° intervals in latitude.
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