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Table 2. Assumed volume sources associated with the deformation of the Sakurajima volcano.

From: Volume change of the magma reservoir relating to the 2011 Kirishima Shinmoe-dake eruption—Charging, discharging and recharging process inferred from GPS measurements

Source type

Location (latitude, longitude, depth)

(beneath Minami-dake, Sakurajima)

   

Isotropic volume source

31.605

130.658

4.0

(beneath the Aira caldera)

   

Isotropic volume source

31.675

130.720

10.0