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中甸春都铜矿区岩体成岩时代及地质意义
引用本文:杨帆,邹国富,吴静,李峰,姜永果,赵向东.中甸春都铜矿区岩体成岩时代及地质意义[J].大地构造与成矿学,2011,35(2):307-314.
作者姓名:杨帆  邹国富  吴静  李峰  姜永果  赵向东
作者单位:昆明理工大学国土资源工程学院;中国有色金属工业昆明勘查设计研究院;
基金项目:校企合作项目(kkk0200921083)资助
摘    要:春都斑岩铜矿床位于中甸铜多金属成矿带的西带南段,矿区主要出露由闪长玢岩和花岗闪长斑岩组成的复式岩体,后者呈岩枝或岩脉产于闪长玢岩体中,并与斑岩铜矿有密切成因关系。本文应用LA-ICP-MS U-Pb定年方法,对闪长玢岩以及花岗闪长斑岩的锆石进行年代学研究。结果表明:岩石中的锆石颗粒为浅黄色-无色透明,呈正方双锥状、柱状的自形晶体,内部发育完好的韵律环带,并具较高的Th/U比值,属典型的岩浆成因锆石;主岩体——闪长玢岩体中的锆石LA-ICP-MS U-Pb年龄为(212±3)Ma,成矿花岗闪长斑岩锆石LA-ICP-MS U-Pb年龄分别为(217±2)Ma和(218±2)Ma。锆石LA-ICP-MS U-Pb年龄数据与地质体穿切关系的矛盾,可能与测试数据较少等因素有关。我们认为,矿区斑岩铜矿的成岩成矿时代均为晚三叠世,与义敦岛弧在237~208Ma之间发生大规模的岛弧岩浆活动相吻合。

关 键 词:成岩时代  地质意义  闪长玢岩  花岗闪长斑岩  春都铜矿  云南中甸

Ages and Geological Significance of the Porphyries in the Chundu Copper Mining Area in Zhongdian,Yunnan Province
YANG Fan,ZOU Guofu,WU Jing,LI Feng,JIANG Yongguo,ZHAO Xiangdong.Ages and Geological Significance of the Porphyries in the Chundu Copper Mining Area in Zhongdian,Yunnan Province[J].Geotectonica et Metallogenia,2011,35(2):307-314.
Authors:YANG Fan  ZOU Guofu  WU Jing  LI Feng  JIANG Yongguo  ZHAO Xiangdong
Institution:YANG Fan1,ZOU Guofu2,WU Jing1,LI Feng1,JIANG Yongguo1 and ZHAO Xiangdong2(1.Department of Land Resources Engineering,Kunming University of Science and Technology,Kunming 650093,Yunnan,China,2.Kunming Institute of Exploration & Design,China Nonferrous Industry Company Ltd,Kunming 650051,China)
Abstract:The Chundu porphyry copper deposit is located at the southern part of the western branch of the Zhongdian copper-polymetallic metallogenic belt. The copper mineralization is closely related to the Chundu granite which consists of diorte-porphyrite and dykes or veins of granodiorite-porphyrite intruded the former. The diorite-porphyrite and granodiorite-porphyry are chronologically dated using zircon LA-ICP-MS U-Pb method. The zircon grains are light yellow to colorless transparent,tetragonal bipyramid cryst...
Keywords:age  geological significance  diorite-porphyrite  granodiorite-porphyry  Chundu porphyry copper deposit  Zhongdian  Yunnan Province  
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