Geological structure and prospects of noble metal ore mineralization of the Khayrkhan gabbroid massif (Western Mongolia) K. R. Kurumshieva, I. F. Gertner, P. A. Tishin
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ArticleSubject(s): Хайрханский габброидный массив | Западная Монголия | благородные металлы | рудоносные горизонтыGenre/Form: статьи в журналах Online resources: Click here to access online
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IOP Conference Series: Earth and Environmental Science Vol. 110. P. 012013 (1-4)Abstract: An analysis of the distribution of noble metals in zones of sulfide mineralization makes it possible to justify the isolation of four ore-bearing horizons with a specific geochemical zonation. A rise in the gold content relative to palladium and platinum is observed from the bottom upwards along the section of the stratified series of gabbroids. The study of the mineral phases of sulphides and the noble minerals itself indicates the evolution of hydrothermal solutions, which determines the different activity and mobility of the fluid (mercury, tellurium, sulfur) and ore (copper, nickel, iron, platinum, gold and silver) components.
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An analysis of the distribution of noble metals in zones of sulfide mineralization makes it possible to justify the isolation of four ore-bearing horizons with a specific geochemical zonation. A rise in the gold content relative to palladium and platinum is observed from the bottom upwards along the section of the stratified series of gabbroids. The study of the mineral phases of sulphides and the noble minerals itself indicates the evolution of hydrothermal solutions, which determines the different activity and mobility of the fluid (mercury, tellurium, sulfur) and ore (copper, nickel, iron, platinum, gold and silver) components.
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