中文摘要:为查明广西大厂锡矿床的成因和成矿物质来源，文章对大厂锡 矿铜坑_长坡矿床不同产出形态的矿体及区内最晚期成矿的茶山锑矿黄铁矿流体包裹体的氦 、氩同位素组成进行了测试。研究结果表明，铜坑_长坡矿床不同产出形态的矿体的成矿流 体氦、氩同位素组成基本一致，3He/4He值为1.2～2.9 Ra，40Ar/36Ar为273～327，反映了成矿流体具有相同来源，且有明显的地幔流体混入；茶山锑矿3He/4He值为0.78 Ra，40Ar/36Ar为268，具岩浆流体与大气水混合特征。
Abstract:To study the genesis and material sources of the Dachang tin deposit, this paper analyzed the helium and argon isotopic components of fluid inclusions in pyrite from different forms of orebodies in the Changpo_Tongkeng deposit and the Chashan Sb deposit which was formed at the last stage. The result indicates that helium and argon isotopic components of the Changpo_Tongkeng deposit are consistent. The 3He/4He ratios are 1.2～2.9 Ra, and the 40Ar/36Ar ratios are 273～327. The data obtained suggest that the Changpo_Tongkeng deposit had the same fluid source, and the mantle fluids were involved in the metallogenic process. The fluids of the Chashan Sb deposit have 3He/4He ratios of 0.78 Ra and 40Ar/36Ar ratios of 268, belonging to the mixture of magmatic fluid and atmospheric water. This reflects the evolutionary trend of metallogenic fluids in the Dachang tin_polymetallic deposit.
keywords:geochemistry, helium_argon isotope, metallogenic fl uid, the Dachang tin_polymetallic deposit
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基金项目:华锡集团有限责任公司博士后工作站科研项目“丹池成矿带构造控矿规律研究"
引用文本：
蔡明海,毛景文，梁 婷，吴付新.2004.广西大厂锡多金属矿床氦、氩同位素特征及其地质意义[J].矿床地质,23(2):225~231.2004.Helium and Argon Isotopic Components of Fluid Inclusions in Dachang Tin_Polyme tallic Deposit and Their Geological Implications[J].Mineral Deposits23(2):225~231
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