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Mineral deposits and chalcogen gases

Published online by Cambridge University Press:  05 July 2018

Martin Hale
Martin Hale*
Affiliation:
International Institute for Aerospace Survey and Earth Sciences, Kanaalweg 3, Delft, Netherlands
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Abstract

Sulphide minerals and their analogues yield gases as a result of oxidation reactions. Even where sulphide minerals are in contact with mildly reducing groundwaters, S2- ions pass into solution and their dispersion patterns can be detected in soil as acid-released H2S. In more oxidising conditions, the metastable gases COS and CS2 are generated. Anomalous dispersion patterns of COS have been reported in soils above more than ten sulphide ore deposits, many of them concealed beneath transported exotic overburden. High concentrations of CS2 occur in the soils over several of the same deposits and uniquely reflect others. Anomalies of SO2 over sulphide deposits are confined to arid terrains. Certain anomalous dispersion patterns of arsenic and tellurium in soils are attributed to the generation and migration of unspecified gases from the oxidation of arsenide and telluride minerals.

Keywords

chalcogen gasessulphide mineralsoxidationarsenictellurium
Type
Geochemistry and Petrology
Information
Mineralogical Magazine , Volume 57 , Issue 389 , December 1993 , pp. 599 - 606
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1993

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References

Boyle, R. W. and Jonasson, I. R. (1973) The geo-chemistry of arsenic and its use as an indicator element in geochemical prospecting. J. Geochem. Explor., 2, 251–96.Google Scholar
Boyle, R. W. and Jonasson, I. R. (1984) The geochemistry of antimony and its use as an indicator element in geochemical prospecting. Ibid. 20, 223-302.Google Scholar
Card, J. W. and Bell, K. (1985) The relationship of soil 210Po and 210Pb geochemical dispersion patterns to uranium mineralization. Ibid., 23, 101-15.Google Scholar
Dyck, W. (1984) Evaluation of the 210Po method at the Midwest uranium deposit, northern Saskatchewan, Canada. Ibid., 20, 85-92.Google Scholar
Henderson, P. (1982) Inorganic Geochemistry. Pergamon Press, 353 pp.Google Scholar
Hinkle, M. E. and Ditbert, C. A. (1984) Gases and trace elements in soils at the North Silver Bell deposit, Pima County, Arizona. J. Geochem. Explor., 20, 323–36.Google Scholar
Hinkle, M. E. and Kantor, J. A., 1978. Collection and analysis of soil gases emanating from buried sulfide mineralization, Johnson Camp area, Coschise Country, Arizona. Ibid., 9, 209-16.Google Scholar
Ryder, J. L., Sutley, S. J., and Botinelly, T., 1990. Production of sulfur gases and carbon dioxide by synthetic weathering of crushed drill cores from the Santa Cruz porphyry copper deposit near Casa Grande, Pinal County, Arizona. Ibid., 38, 43-67.Google Scholar
Jin, Jun, Hu, Zhengqing, Sun, Xiangli, Zhang, Maozhong, and Zhan, Meidi (1989) Geochemical exploration in thick transported overburden, eastern China. Ibid., 33, 155-69.Google Scholar
Kesler, S. E. and Gardner, M. (1986) Factors affecting sulfur gas anomalies in overburden. J. Geophys. Res., 91, 12,339-42.Google Scholar
Kesler, S. E. Gerdenich, M. J., Steininger, R. C., and Smith, C. (1990) Dispersion of soil gas around micron gold deposits. J. Geochem. Explor., 38, 117–32.Google Scholar
Lakin, H. W., 1972. Selenium accumulation in soils and its adsorption by plants and animals. Bull. Geol. Soc. Amer., 83, 181–90.Google Scholar
Levinson, A. A. (1980) Introduction to exploration geochemistry. Applied Pub., 924 pp.Google Scholar
Lovell, J. S., Hale, M. and Webb, J. S. (1980) Vapour geochemistry in mineral exploration. Mineral. Mag., 143, 229–39.Google Scholar
Nicholson, R. A., Peachey, D. and Ball, T. K. (1988) Tests on use of sulphur gases in soils to detect hidden mineralization. Trans. lnstn. Min. Metall., 971, B57-63.Google Scholar
Oakes, B. W. (1984) Vapour geochemical pathfinders for oxidizing sulphide mineralization beneath exotic overburden. Unpub. PhD thesis, Univ. of London, 350 pp.Google Scholar
Oakes, B. W. and Hale, M. (1987) Dispersion patterns of carbonyl sulphide above mineral deposits. J. Geochem. Explor., 28, 23549.Google Scholar
Plant, J. A., Breward, N., Forrest, M. D. and Smith, R. T., (1989) The gold pathfinder elements As, Sb and Bi—their distribution and significance in the southwest Highlands of Scotland. Trans. Instn. Min. Metall., 98, B91-101.Google Scholar
Rose, A. W., Hawkes, H. E. and Webb, J. S. (1979) Geochemistry in mineral exploration. Academic Press, 657 pp.Google Scholar
Ruan, T., (1982) Some new approaches in vapour geochemistry. Unpub. rep., Imp. Coll. Sci. Techl., London.Google Scholar
Taylor, C. H., Kesler, S. E. and Cloke, P. L. (1982) Sulfur gases produced by the decomposition of sulfide minerals; application to geochemical exploration. J. Geochem. Explor., 17, 165–85.Google Scholar
Watterson, J. R., Gott, G. B., Neuerburg, G. J., Lakin, H. W. and Cathrall, J. B. (1977) Tellurium, a guide to mineral deposits. Ibid. 8, 31-48.Google Scholar