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In consideration of the small number of polarity data from the OBSs, earthquakes which did not have a unique focal solution were not considered.
The occurrence time is shown at the top of each focal solution, and the magnitude and score are shown at the bottom where "score" means a ratio of the data consistent to the obtained solution to the total data.
If there were plural focal solution candidates with the same best score for a event, the best solution was chosen so that the polarities consistent with that solution were located farthest away from the nodal planes and the polarities inconsistent with the solution were closest to one of the planes.
After aftershocks from the quake had concluded, examination took place, producing a focal solution to the small events.
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In addition, we selected 31 events which correspond to our results from the catalog of focal solutions determined by the automated moment tensor determination, using Japanese land seismic network data (F-net) (Fukuyama et al., 1998).
The average SHmax orientation in wells B, C, D and E in the Kelasu Belt correspond to 124.76°N (±8.5°), 92.86°N (±4.3°), 143.28°N (±7.1°) and 180.89°N (±4.5°), respectively, which coincides well with the result derived from the focal mechanism solution.
The field observations of the MSR supported this focal mechanism solution.
We calculate the ΔCFF values for two nodal planes of each focal mechanism solution.
We then prepare two spatially gridded matrices for both nodal planes of the focal mechanism solution.
The focal mechanism solution of earthquakes in the BG area is a mixture of strike-slip and normal faulting with predominant strike-slip focal mechanism solution (Delouis et al., 2002; Fig.2002
Moreover, a focal mechanism solution of aftershocks provides additional information associated with the orientation of the fault plane.
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