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Fluid ascent is suggested by a pressure source and clustered seismicity.
The fumarole in the Da-you-keng area originates from vapor-dominant hydrothermal fluids that may be supplied from a deeper part beneath Cing-tian-gang, suggested by a pressure source and low to relatively low resistivity.
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Uplift event 1 was caused by the appearance of a pressure source and dike intrusion associated with the AD 2000 eruption of Miyakejima Volcano.
These uplift events were caused by the development of a pressure source beneath Kouzushima and dike intrusion associated with the AD 2000 eruption of Miyakejima Volcano, respectively (Kimata et al. 2000; Murakami et al. 2001; Nishimura et al. 2001; Yamaoka et al. 2005).
Beneath this region, there are 'spasmodic bursts' of clustered seismicity inferred by the seismological observations of Konstantinou et al. ([2007]) and a pressure source inferred by Murase et al. ([2013])'s precise leveling surveys, as shown in Figure 6.
The underlying low to relatively low resistivity region R3 beneath Cing-tian-gang corresponds to a pressure source inferred by Murase et al. ([2013]).
We interpret this change as having been caused by a shallow pressure source.
A central pressure source is provided by a high-pressure storage unit with an integrated valve, which provides ingress gas flow to the system; the gas is then routed through the system via a sequence of valve operations and cellular actuations, allowing for any desired shape to be achieved within the constraints of the deployed array geometry.
The developed overall structure is made up of a number of cellular colonies, each consisting of a central pressure source surrounded by multiple cells.
Miyaoka and Takagi (2016) showed that the 2014 eruption was preceded by slight inflation of a deep pressure source at unspecified depth, beginning less than 1 month before the eruption.
We examined two source types, a spherical pressure source and a tensile crack source.
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