Research Article

Implications of Self-Potential Distribution for Groundwater Flow System in a Nonvolcanic Mountain Slope

Figure 5

(a) The observed raw SP profile (gray line with diamonds) and low-pass filtered one called as “regional” pattern in this study (solid line). (b) Residual SP profile after subtracting regional SP from raw data, called as “local” anomalies.
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(a)
640250.fig.005b
(b)