Table 4 The Osnabr\(\ddot{{u}}\)ck 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

0.9931

0.6

0.9946

0.7

0.9938

0.8

0.9931

0.9

0.9948

1.0

0.9962

1.1

0.9972

1.2

0.9976

1.3

0.9974

1.4

0.9969

1.5

0.9959

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