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Geoelectrochemical exploration

The methods of geoelectrochemical exploration are based on investigation of the polarisation curve (voltammogram), which records the dependence of a current through an electronic conductor on its electrode potential. The electrode potential of an electronic conductor is its potential measured with respect to an auxiliary standard non-polarisable electrode which is immersed in the host ionic conductor in direct contact with the surface of the electronic conductor. [Pg.53]

Putikov, O F., 1987. Theoretical basis of the geoelectrochemical exploration methods. Leningrad State University Press, Leningrad, 176 pp. (in Russian). [Pg.498]

Alekseev, S.G., Dukhanin, A.S., Veshcv, S.A. and Voroshilov, N.A., 1996. Some aspects of practical use of geoelectrochemical methods of exploration for deep-seated mineralisation. J. Geochem. [Pg.471]

Karar, V.P.and Sakovich, B.B., 1989. Application of the CHIM method for prospecting placer gold deposits at the Enisey mountain-ridge. Application of Geoelectrochemical methods for Prospecting and Exploration of Ore Deposits. NPO Rudgeofizika, Leningrad, pp. 189-112 (in Russian). [Pg.489]

Ryss, Yu.S., 1983. Geoelectrochemical Methods of Exploration (Introduction to Geoelectrochemistry). Nedra, Leningrad, 255 pp. (in Russian). [Pg.502]


See other pages where Geoelectrochemical exploration is mentioned: [Pg.53]    [Pg.53]    [Pg.17]    [Pg.79]    [Pg.79]    [Pg.474]    [Pg.490]    [Pg.502]    [Pg.564]   
See also in sourсe #XX -- [ Pg.17 , Pg.19 , Pg.43 , Pg.53 , Pg.67 , Pg.78 , Pg.79 ]




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