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Abstract

Different theories have been proposed for modelling self potential anomalies appearing in connection with sulphide and graphite deposits. Most common models have been based on volume distributions of dipole sources, which have been used analogically with magnetic modelling.

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/content/papers/10.3997/2214-4609.201411528
1993-06-08
2024-04-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201411528
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