中文摘要:文章从碳、氢、氧、硫、铅、锶等同位素地球化学方面探讨了湘中锑金矿床的成矿物质与成矿流体来源。研究表明：湘中盆地中锑矿床的碳、硫等矿化剂主要来源于基底地层，而盆地边缘锑(金)矿床的碳、硫等矿化剂来源于深部岩浆作用；Au，Sb等成矿物质都来源于基底碎屑岩；成矿流体主要为大气降水。
Abstract:Central Hunan area is a world_famous area for Sb (Au) mineralization. This paper has systematically studied carbon, hydrogen, oxygen, sulfur, lead and strontium isotopic geochemical characteristics of Sb (Au) deposits in central Hunan and discussed sources of ore_forming metals and ore_forming fluids. The researches show that the ore_forming metals such as Sb and Au came from basement clastics, while the ore_forming fluids were mainly derived from meteoric water.
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基金项目:科技部国家重点基础研究项目(G1999043210)、国家自然科学基金重点项目(49733012)及教育部博士点基金(98028422)
引用文本：
马东升，潘家永，解庆林.2003.湘中锑(金)矿床成矿物质来源——Ⅱ.同位素地球化学证据[J].矿床地质,22(1):78~87.2003.Ore Sources of Sb(Au) Deposits in Central Hunan：Ⅱ. Evidence of Isotopic Geochemistry[J].Mineral Deposits22(1):78~87
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