Table 10 The Bavarian woods self-potential anomaly, Germany. R-max versus q.

From: A fast imaging method for the interpretation of self-potential data with application to geothermal systems and mineral investigation

q

R-max

0.5

0.9583

0.6

0.9783

0.7

0.9929

0.8

0.9978

0.94

0.9983

1.0

0.9979

1.1

0.9974

1.2

0.9974

1.3

0.9965

1.4

0.9941

1.5

0.9911

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