| 澳大利亚纳沃日金矿流体混合与金的成矿作用 |
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| 引用本文： | 范宏瑞,D I Groves,E J Mikuckj,N J McNaughton.澳大利亚纳沃日金矿流体混合与金的成矿作用[J].矿床地质,2001,20(1):37-43. |
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| 作者姓名： | 范宏瑞 D I Groves E J Mikuckj N J McNaughton |
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| 作者单位： | 1. 中国科学院地质与地球物理研究所,
2. 西澳大利亚大学地质与地球物理系矿床教学研究中心,珀斯,澳大利亚 |
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| 摘 要： | 流体包裹体研究表明，纳沃日金矿成矿脉体中流体包裹体类型有三种，富CH4、CH4－CO2－H2O和富H2O包裹体。初始成矿流体是富CH4热液，在主矿化阶段，另一来源的CO2－H2O流体与CH4流体发生了不均匀混合，并且在石英－磁黄铁矿阶段最为强烈，造成不同矿化部位的xCH4变化极大，早期近于纯CH4流体被充分“稀释”后，石英－黄铁矿阶段的xCH4显著减小，到成矿晚期只剩CO2－H2O流体。正是由于不同性质流体的混合，造成热液的pH及fo2的升高，流体中的金－硫络合物分解，金沉淀成矿。
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| 关 键 词： | 成矿热液 成矿作用 西澳大利亚 金矿床 矿区地质 流体包裹体 |
| 文章编号： | 0258-7106(2001)01-0037-07 |
Fluid Mixing in the Generation of Nevoria Gold Mineralisation in the Southern Cross Greenstone Belt, Western Australia |
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| FAN Hongrui,D.I.Groves,E.J.Mikucki,N.J.McNaughton.Fluid Mixing in the Generation of Nevoria Gold Mineralisation in the Southern Cross Greenstone Belt, Western Australia[J].Mineral Deposits,2001,20(1):37-43. |
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| Authors: | FAN Hongrui DIGroves EJMikucki NJMcNaughton |
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| Abstract: | The Nevoria deposit, a banded iron formation-hosted gold deposit, occurs within the roof of amphibolite-facies greenstones in the Southern Cross belt, Yilgarn Block, Western Australia. The mineralizing veins include early quartz-pyrrhotite+ chalcopyrite veins and late quartz- pyrite veins. Three types of fluid inclusions, namely CH4-rich, CH4-CO2-H2O and H2O-rich ones, were found at Nevoria. Microthermometric data reveal that the initial auriferous fluids were CH4-dominant. Fluid mixing may have caused remarkable variations of CH4/CO2 ratios or XCH4 of CH4-CO2-H2O inclusions, particularly in mineralized quartz-pyrrhotite veins. The CH4-C02-H2O inclusions in quartz-pyrite vein set have an apparent trend of decreasing XCH4 and increasing molar volume.It can be inferred that, from the quartz-pyrrhotite stage to the quartz-pyrite stage, homogenization temperatures of CH4-CO2-H2O inclusions decreased, and CH4 contents ( XCH4) also decreased. The carbonic phase in the inclusions varies from CH4-dominant to CO2-dominant. Phase mixing, resulting in an increase in pH and toz, together with loss of reduced sulfur by mineral/fluid reactions and precipitation of sulfides, led to the breakdown of the gold-transporting complexes. |
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| Keywords: | Fluid mixing ore forming-fluid gold mineralization Nevoria western Australia |
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