International Journal of Geophysics / 2012 / Article / Fig 6

Research Article

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

Figure 6

Calculated SP from various depths of a point source (1–100 m). The SP values are normalized by the respective value at 0 m in the horizontal distance where the source is located. The observed SP anomalies “A” and “B” in Figure 5(b) are shown by circles and rectangles, respectively.

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