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Geochemical Characteristics of Tianmashan Au-S Deposit in Tongling, Anhui Province, China

机译:中国安徽省铜陵天马山AU-S矿床地球化学特征

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The Tianmashan Au-S deposit is geochemically characterized by a vertical variation and a two-layer texture as well as the development of the upper stratiform ore bodies and the lower net-stockwork ores. Pb, Zn, Au, Ag, As, Hg contents and average δ~(18)O values increase progressively whereas Cu, Mo, Cr, Co, Ni, REE contents and δ~(34)S decrease gradually from the lower net-stockwork ores to the upper stratiform ores. δ~(34)S values of pyrite range from +4.0%o to +9.6%o. The average δ~(18)O value of calcite and quartz in the upper stratiform ores is +13.7%o, while that of quartz and whole rock in the lower net-stockwork ores is + 12.3%o. These geochemical characteristics suggest that the Tianmashan Au-S deposit is of the submarine sedimentary exhalative origin.
机译:Tianmashan Au-S沉积物是通过垂直变化和双层纹理的地球化学特征以及上层矿体和下净袜子矿石的开发。 Pb,Zn,Au,Ag,As,Hg含量和平均Δ〜(18)O值逐渐增加,而Cu,Mo,Cr,Co,Ni,Ree含量和Δ〜(34)S逐渐从下部逐渐降低 - 上层矿石的影像矿石。 δ〜(34)硫铁矿的值范围为+ 4.0%O至+ 9.6%O。方层型矿石中方解石和石英的平均δ〜(18)o值为+ 13.7%O,而石英和整个岩石在下部净袜子矿石中的含量为+ 12.3%o。这些地球化学特征表明,天马山AU-S押金是潜艇沉积呼气起源。

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