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太白金礦載金礦物標形特征

Characteristics of Ore-Bearing Mineral and Its Genesis Significance of Taibai Gold Deposit

  • 摘要: 太白金礦的礦化共經歷了4個成礦階段,其中黃鐵礦-含鐵白云石階段是最重要的金礦化階段.黃鐵礦為主要載金礦物.黃鐵礦中鉑的含量與Au+Ag含量呈負相關,金礦物主要以微米級的自然金產于Ⅱ,Ⅳ階段的黃鐵礦中,成色879~965,金的成色總體上向深部直升高的趨勢.自然金中鉑含量與金的成色呈負相關.黃鐵礦中有高的Pt含量和Te含量.黃鐵礦具有混合導型特點,δ34S值為6.5×10-3~11.6×10-3

     

    Abstract: According to electron probe analysis of 12 samples, As, Se, Ni, Au, Pt were detected as trace element in pyrite. Pt content is negahve correlated with Au+Ag content The native gold is closely associated with pyrite from stage 2 and stage 4. It occurs is the, fissure filling or on the crystal boundary of pyrite.The finess of gold is falling from 1290 level to 1350 level, which indicated that the ore-forming temperature is from high (downside) to low (upside). Pt content is negahve cormlated with the finess of gold. High Pt and Te content indicated that the ore forming of this deposit is related with abyssal magmatism. Pt content of pyrite is not only genesis significance but also of significance of explorahon.

     

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