University of New Brunswick

Laboratory and field evidence in support of the electrogeochemically enhanced migration of ions through glaciolacustrine sediment

University of New Brunswick
04/09/1983      Smee, B.W.     

Ph.D. Thesis, Univ. New Brunswick. 477 p.

Abstract

Ionic aureoles, overlying or contiguous to massive sulphide occurrences, are postulated to have been emplaced as a result of natural galvanic forces. The occurrences of these galvanic forces, most commonly referred to as the self-potential or spontaneous polarization phenomena, are well documented, but ionic migration in response to these electrical forces remained to be proven conclusively.


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