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We demonstrate that a VAOL-5GSBY4 LED (λdominant = 460 nm) can be used as a dynamic trigger to vary the level of NO released from 500 μm diameter coated PMMA.
Although their assumed geometry was different from the fault zones in Kumamoto and Oita, extended simulations would be helpful for understanding the cause of dynamic trigger in Oita area, where hydrothermal effects probably played an important role.
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Note that we did not use seismic stations in Oita prefecture to avoid possible contamination by a dynamically triggered event discussed in "Dynamic triggering in Yufuin Beppu area" section.
It is known that some swarm activities start as a result of delayed dynamic triggering and other swam activities start from a dynamically triggered event by passing waves and persist for certain period (e.g., Hill et al. 1993).
A return to low seismicity levels 1 month after the triggered earthquake may have important implications for seismic hazard due to dynamic triggering.
The ubiquitous nature of dynamic triggering.
Gomberg, J. Permanently enhanced dynamic triggering probabilities as evidenced by two M > 7.5 earthquakes.
Wallace, L. M. et al. Large-scale dynamic triggering of shallow slow slip enhanced by overlying sedimentary wedge.
Shelly, D. R., Peng, Z. G., Hill, D. P. & Aiken, C. Triggered creep as a possible mechanism for delayed dynamic triggering of tremor and earthquakes.
Johnson, C. W., R. Bürgmann, and F. F. Pollitz (2015), Rare dynamic triggering of remote M≥ 5.5 earthquakes from global catalog analysis, J. Geophys.
Johnson, C. W., and R. Bürgmann (2016), Delayed dynamic triggering: Local seismicity leading up to three remote M≥6 aftershocks of the 11 April 2012 M8.6 Indian Ocean earthquake, J. Geophys.
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