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新疆包古图斑岩铜矿矿床地质特征

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宋会侠 刘玉琳 屈文俊 宋彪 张锐 成勇. 新疆包古图斑岩铜矿矿床地质特征[J]. 岩石学报, 2007, 23(8): 1981-1988.
引用本文: 宋会侠 刘玉琳 屈文俊 宋彪 张锐 成勇. 新疆包古图斑岩铜矿矿床地质特征[J]. 岩石学报, 2007, 23(8): 1981-1988.
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SONG HuiXia, LIU YuLin, QU WenJun, SONG Biao, ZHANG Rui, CHENG Yong. Geological characters of Baogutu porphyry copper deposit in Xinjiang, NW China[J]. Acta Petrologica Sinica, 2007, 23(8): 1981-1988.
Citation: SONG HuiXia, LIU YuLin, QU WenJun, SONG Biao, ZHANG Rui, CHENG Yong. Geological characters of Baogutu porphyry copper deposit in Xinjiang, NW China[J]. Acta Petrologica Sinica, 2007, 23(8): 1981-1988.
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新疆包古图斑岩铜矿矿床地质特征

    • [1]中国地质科学院地质研究所,北京100037 [2]北京大学地球与空间科学学院,北京100871 [3]北京离子探针中心,北京100037 [4]国家地质实验测试中心,北京100037 [5]新疆有色地质勘查局地质研究所,乌鲁木齐830000

  • 基金项目:

    地质调查项目（1212010531002）资助.致谢本论文的野外工作得到新疆有色地质勘查局地质研究所工作人员的大力帮助,沈其韩院士、王彦斌研究员和朱永峰教授提出了宝贵意见,在此表示感谢!

Geological characters of Baogutu porphyry copper deposit in Xinjiang, NW China

    • 1.Institute of Geology, Chinese Academy of Geological sciences, Beijing 100037, China;2. School of Earth and Space Sciences, Peking University, Beijing 100871, China;3. Laboratory of SHRIMP Beijing, Beijing 100037, China;4. National Research Center of Geoanalysis, Beijing 100037, China;5. Geological Institute, Xinjiang Geoexploration Bureau for Non-ferrous Metals, Urumchi 830000, China

    摘要
  • 新发现的包古图斑岩铜矿床位于准噶尔盆地西缘，达尔布特断裂以南的包古图地区。通过对V号主要赋矿岩体及钻孔岩心的野外和镜下观察，研究了矿体矿化情况、蚀变分带特征和矿石组合。对该矿床的流体包裹体分类研究表明，主成矿期成矿温度在180℃～450℃，包裹体的形成压力多在1～9MPa。由此得出的斑岩体的侵位深度在100～600m。黄铜矿和黄铁矿的δ^34S变化范围分别是-2.4‰～-0.8％o和-2.7‰～＋0.7‰。对该矿床的初步研究认为，矿床是在埃达克质岩浆侵位到地壳浅部冷却成岩后，经历了两期含矿热液的作用而成矿的。早期形成Cu、Fe、Mo、Zn的硫化物矿物，可划分为4个成矿阶段；晚期形成Cu-Te-Bi-Au-Ag的复杂矿物组合。早期矿化形成的辉钼矿Re-0s年龄是310Ma。
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修回日期:  2007-04-21
刊出日期:  2007-08-31

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