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Fig. 14 | Earth, Planets and Space

Fig. 14

From: Magma reservoir beneath Azumayama Volcano, NE Japan, as inferred from a three-dimensional electrical resistivity model explored by means of magnetotelluric method

Fig. 14

F-statistic change of each site in terms of resistivity change of target area shown in Fig. 13. a F-statistic change obtained by changing resistivity inside isosurface in Fig. 13a. b Same with (a), but obtained by changing resistivity inside Fig. 13b. The confidence levels of 95, 90, and 67% are shown in blue, red, and green lines, respectively. The 67 to 95% CIR in a are not available. The 67% and 90% CIR in b are determined to be 0.3 to 5 Ωm (dark shade) and 0.02 to 70 Ωm (light shade), respectively

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