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The specific seismic source mechanisms associated with reservoir induction have been established in a few cases.
This direct capture is the first of three source mechanisms that can be described.
Two source mechanisms are found near the step.
Strike and rake angles of source mechanisms are the same for all three sources.
We performed waveform inversion of the VLP event assuming several candidate source mechanisms.
Among the four candidate source mechanisms, a tensile crack yielded the minimum AIC value (Table 2).
The event source mechanisms are the moment tensor solutions from F-net (Okada et al. 2004).
We selected these events to include a variety of source mechanisms.
Table 2 Comparison of Akaike Information Criterion (AIC) values among the four assumed source mechanisms.
Non-DC source mechanisms have also been reported in induced seismicity.
We discuss the source mechanisms and the possible meanings of these two different compound microstructures.
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