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Fig. 4. Results of stress tensor inversion by the multiple inverse method.
We examined the focal mechanism distributions before and after the Tohoku earthquake and performed a stress tensor inversion using a multiple inverse method (Otsubo et al., 2008).
We investigated the focal mechanism distributions using the dataset obtained by the F-net over a longer time duration after the mainshock than Asano et al. (2011), and performed the stress tensor inversion by the multiple inverse method (Otsubo et al., 2008).
The multiple inverse method of stress tensor inversion detected two normal-faulting stress states that dominate in different regions.
The multiple inverse method (MIM) of stress inversion resolves statistically significant stress heterogeneities in the study area.
In the stress tensor inversion, we used the multiple inverse method (Yamaji, 2000; Otsubo et al., 2008), which uses a resampling technique to separate spatiotemporal plural stress states.
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The method combines experimental measurements of the normal hemispherical transmittance and reflectance of the suspensions in conventional cuvettes with an inverse method and analytical expressions obtained from the modified two-flux approximation accounting for absorption and multiple scattering.
In the inverse method, the bowls would keep their traditional alliances.
The inverse method also gives every major bowl a chance to stay relevant every year.
The other method, which is known as the inverse method, is a bit more complicated and appeases more parties.
Through various investigations, it is shown that the developed inverse method and scaling relationships can serve as effective and accurate tools in the prediction of open-hole compression and compression after impact strengths for multiple layups of different material systems.
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