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(b) Interpretation of the resistivity structure.
Figure 6(b) shows the interpretation of the resistivity structure.
As inferred by interpretation of the resistivity structure and other geochemical and geophysical evidence.
An interpretation of the resistivity model is presented in Fig. 5(b) where a domal structure develops through the underplating of sediments which 'jack-up' the units above.
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Although the interpretation of the low resistivity is still ambiguous, one can interpret the low resistivity as indication of high temperature area, because, relatively high geothermal gradient (40 90 K/km around 1 km of depth) was observed in Mt. Aso (Tanaka et al. 2004a, b).
These studies on fumarolic gases infer that the granitic basement is located at shallow levels, which is consistent with our interpretation of the high resistivity layer.
For interpretation of VES data for hydrogeological characterisation, quantitative and qualitative methods of interpretation of the field apparent resistivity data were employed (Murali and Patangay 2006).
Because the main characteristics of the inferred resistivity structure remained stable throughout the entire observation period (Fig. 9), it is possible to make meaningful geological interpretations of this resistivity structure.
The estimation of humidity in the unsaturated zone of soils and NAPL saturation in contaminated aquifers may be based on the interpretation of electrical resistivity index logs.
The most important area to consider in interpretation is the area of the resistivity decrease between 500 and 700 m, as the other resistivity changes in the model are much smaller and should not be overinterpreted.
With regard to the electrical logging technology in the petroleum industry, almost all research has focused on the detection and interpretation of formation resistivity.
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