矿床地质:2015,Vol.>>Issue(2):289-308

黑龙江省铜山铜矿床英云闪长岩锆石U-Pb年龄及地球化学特征
中国地质科学院矿产资源研究所 国土资源部成矿作用与资源评价重点实验室, 北京 100037;中国地质科学院矿产资源研究所 国土资源部成矿作用与资源评价重点实验室, 北京 100037;中国地质博物馆, 北京 100034;中国地质大学, 北京 100083;中国地质科学院矿产资源研究所 国土资源部成矿作用与资源评价重点实验室, 北京 100037
Zircon U-Pb dating and geochemistry of ore-bearing tonalite in Tongshan copper deposit, Heilongjiang Province
LIU Jun,ZHOU ZhenHua,HE ZheFeng,OUYANG HeGen
(MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China;Geological Museum of China, Beijing 100034, China;China University of Geosciences, Beijing 100083, China)
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投稿时间:2014-07-26   修订日期:2014-10-01      网络发布日期:2015-05-06
中文摘要:铜山矿床是位于大兴安岭北段多宝山矿田中的一个大型铜矿床。文章对该矿区含矿英云闪长岩进行了详细的LA-MC-ICP-MS锆石U-Pb定年、主量元素、微量元素及同位素地球化学研究。锆石U-Pb定年结果表明, 英云闪长岩侵位于(461±1) Ma。岩石显示埃达克质岩的地球化学特征, 具有高w(SiO2)(62.5%~64.53%)和w(Al2O3)(14.77% ~ 17.7%), 高w(Sr)(394×10-6 ~ 804×10-6), 低w(Y)(7.78×10-6 ~ 10.3×10-6)和w(Yb)(0.8×10-6 ~ 1.04×10-6), 轻稀土元素富集, 重稀土元素亏损, 无明显Eu异常。锆石εHf(t)值介于11.6 ~ 13.5。金属硫化物的δ34S值为-1.3‰ ~ -0.4‰, 206Pb/204Pb、207Pb/204Pb和208Pb/204Pb值分别为17.591~18.453、15.449~ 15.551和37.280~37.999。这些特征表明, 铜山矿床英云闪长岩形成于大陆边缘弧环境, 是加厚下地壳部分熔融的产物。成矿物质主要来自于英云闪长岩及多宝山组火山岩。
Abstract:The Tongshan deposit is a large copper deposit located in the Duobaoshan orefield within the northern Da Hinggan Mountains. This paper reports LA-MC-ICP-MS zircon U-Pb age, major and trace elements, and isotopic geochemistry of the ore-related tonalite in the Tongshan deposit. LA-MC-ICP-MS zircon U-Pb dating yielded the crystallization age of (461±1) Ma for the tonalite. The tonalite shows characteristics of adakitic affinity, i.e., high SiO2 (62.5% ~ 64.53%), Al2O3 (14.77%~17.7%) and Sr (394×10-6 ~ 804×10-6), low Y (7.78×10-6 ~10.3×10-6) and Yb (0.8×10-6 ~ 1.04×10-6), slight Eu anomalies, rich light rare-earth elements and depleted heavy rare-earth elements. The zircon Hf isotope analysis shows εHf(t) values of 11.6 to 13.5. δ34S values of sulfides are between -1.3‰ and -0.4‰, similar to data associated with magmatic-hydrothermal systems. 206Pb/204Pb, 207Pb/204Pb and 208Pb/204Pb ratios vary from 17.591 to 18.453, 15.449 to 15.551, and 37.280 to 37.999, respectively. The tonalite was formed in a continental marginal arc setting, and originated from partial melting of the thickened lower crust. The ore-forming materials were derived from the volcanic rocks of the Duobaoshan Formation and tonalite.
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中图分类号:P618.41;P597     
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基金项目:本文得到中国地质调查局地质调查项目(12120113093600)和国家自然科学基金项目(41172081)联合资助
引用文本:
刘军,周振华,何哲峰,欧阳荷根.2015.黑龙江省铜山铜矿床英云闪长岩锆石U-Pb年龄及地球化学特征[J].矿床地质,34(2):289~308
LIU Jun,ZHOU ZhenHua,HE ZheFeng,OUYANG HeGen.2015.Zircon U-Pb dating and geochemistry of ore-bearing tonalite in Tongshan copper deposit, Heilongjiang Province[J].Mineral Deposits34(2):289~308
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