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The orange part of the trace indicates the conduit zone defined by Nakada et al. (2005).
The yellow area is the conduit zone inferred from our results and previous studies.
The conduit zone contains multiple dykes of different ages, including materials deposited during the latest 1990 1995 eruption.
The conduit zone is located away from the undulation structure in the reflection section towards the south.
In this figure, the USDP-4 trace, shown in orange, corresponds to the conduit zone reported by Nakada et al. (2005).
According to the results of a drilling project the Unzen Scientific Drilling Project USDPP)—many dykes and veins of different compositions had intruded into the conduit zone beneath the lava dome (Nakada et al., 2005).
Similar(52)
presence and stress components of fractures; as conduit zones.
However, Matsubara et al. (2000) detected a small (—5 km) conduit-like zone of low P-wave velocity (4.1 5.5 km/s) and high V p /V s (1.8 2.7) in the upper crust immediately below Tateyama, and interpreted it caused by partially molten material with a fluid fraction of 5 15%.
On March 5, increasing pressurization of the east rift zone conduit reached the failure point, and magma intruded from the conduit to the surface, triggering the Kamoamoa fissure eruption (Orr et al. 2013b).
For Regions 1 and 2, horizontal permeability is ten times greater than vertical, and in the conduit and sealing zone permeability is isotropic.
On August 3, fissures opened on the lower flank of Pu'u 'Ō'ō, again depressurizing the east rift zone conduit and leading to a rapid drop (of about 85 m) in the Halema'uma'u lava lake.
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