|
Absolute Value of
|
Comparison of Stress Models
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| Coulomb Stress | Effective Number of | Significance of |
Static Coulomb Stress
|
Control Stress Model (5)
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| Change | M"e2.6 Observations | Correlation (%) (3) | Percent Agreement | Significance | Percent Agreement | Significance | ||||||||
| (bars) | N | Agree(1) | Disagree(2) | with Seismicity (1) | (%) (4) | with Seismicity (1) | (%) (4) | |||||||
| "d 8.0 | 193 | 118 | 75 | 6.4 | 98 | 61 | 99.9 | 60 | 99.9 | |||||
| "d 2.0 | 184 | 110 | 74 | 4.9 | 97 | 60 | 97 | 58 | 98 | |||||
| "d 1.0 | 181 | 107 | 74 | 4.3 | 96 | 59 | 98 | 55 | 90 | |||||
| "d 0.5 | 170 | 97 | 73 | 2.0 | 84 | 57 | 97 | 53 | 78 | |||||
| "d 0.2 | 135 | 78 | 57 | 1.2 | 72 | 58 | 97 | 53 | 73 | |||||
1) Seismicity rate and model stress both increase or both decrease.
2) Seismicity rate and model stress change in opposite directions.
3) Based on
test.
4) Based on binomial test.
5) Control stress model in which stress change is Dt(1/(d+1)),
where d is distance (km) from the Nojima - Rokko fault trace, and Dt
is the static shear stress drop on the fault.