| 黑龙江多宝山斑岩Cu-Mo矿床成岩成矿时代研究 |
| Received:November 17, 2011 Revised:November 01, 2012 点此下载全文 |
| 引用本文：XIANG AnPing,YANG YunCheng,LI GuiTao,SHE HongQuan,GUAN JiDong,LI JinWen,GUO ZhiJun.2012.Diagenetic and metallogenic ages of Duobaoshan porphyry Cu-Mo deposit in Heilongjiang Province[J].Mineral Deposits,31(6):1237~1248 |
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| Author Name | Affiliation | E-mail | | XIANG AnPing | MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China | | | YANG YunCheng | MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China | | | LI GuiTao | Inner Mongolia Bureau of Geology and Mineral Resources Development, Hohhot 010020, Inner Mongolia, China | | | SHE HongQuan | MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China | shehongquan@sina.com | | GUAN JiDong | No.6 Institute of Geology and Mineral Exploration of Inner Mongolia, Hailar 021008, Inner Mongolia, China | | | LI JinWen | MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China | | | GUO ZhiJun | MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China | |
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| 基金项目:本文为地质调查项目(N1014)、"十一五"国家科技支撑计划重大项目(编号: 2006BAB01A10)和国家基础科研项目(编号: 2013CB429800)联合资助成果 |
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| 中文摘要:多宝山斑岩型铜(钼)矿床是中国东北地区重要的斑岩型铜(钼)矿床,文章对矿区主要成矿岩体及辉钼矿样品进行了系统的成岩成矿年代学研究。对成矿岩体采用高精度LA-ICP-MS锆石U-Pb测年,获得成矿母岩花岗闪长斑岩的锆石U-Pb年龄为(474.8±4.7) Ma,矿体寄主岩石花岗闪长岩的锆石U-Pb年龄为(478.1±4.1) Ma,以及矿体外围黑云母花岗闪长岩的锆石U-Pb年龄为(483.9±4.5) Ma;矿体辉钼矿的Re-Os同位素模式年龄加权平均值为(475.1±5.1) Ma。测年结果显示,多宝山斑岩铜(钼)矿床形成于早奥陶世。结合含矿地层、矿区岩石组合特征,以及前人研究的岩石地球化学特征,推测多宝山矿床形成于早奥陶世与板块俯冲有关的岛弧环境,说明在区域上寻找类似多宝山的斑岩铜矿应沿早奥陶世多宝山-伊尔斯岩浆岛弧带开展。 |
| 中文关键词:地球化学 LA-ICP-MS锆石U-Pb测年 Re-Os测年 岛弧 多宝山斑岩型铜(钼)矿床 |
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| Diagenetic and metallogenic ages of Duobaoshan porphyry Cu-Mo deposit in Heilongjiang Province |
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| Abstract:The Duobaoshan porphyry Cu-Mo deposit is an important Cu deposit in Northeast China. Systematic isotope dating was conducted to determine the metallogenic age of the deposit. LA-ICP-MS zircon U-Pb dating indicates that the parent granite-porphyry rocks and the host rocks intruded at (474.8±4.7) Ma and (478.1±4.1) Ma, respectively, the biotite granodiorite outside the parent granite-porphyry was formed at (483.9±4.5) Ma. Meanwhile, seven Re-Os isotopic analyses of molybdenite yield a weighted average model age of (475.1±5.1) Ma. These data show that the ore-forming process and the intrusion of the host rocks were completed in the early Ordovician. According to the ages of mineralization and intrusion of host rocks, the sedimentary setting of the Duobaoshan Formation and the geochemical characteristics of rocks hosting the deposit, the authors hold that the porphyry Cu-Mo deposit was formed in an island arc regime related to plate subduction in the Early Ordovician, and that the prospecting direction for such a type of porphyry copper deposits should be in the magma island arc belt distributed in Duobaoshan-Yi'ershi area. |
| keywords:geochemistry LA-ICP-MS zircon U-Pb dating Re-Os dating island arc Duobaoshan porphyry Cu-Mo deposit |
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