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拉拉铜矿含矿岩系地球化学特征及其构造意义
引用本文:周家云,郑荣才,朱志敏,陈家彪,沈冰,李潇雨,罗丽萍.拉拉铜矿含矿岩系地球化学特征及其构造意义[J].矿产与地质,2009,23(2).
作者姓名:周家云  郑荣才  朱志敏  陈家彪  沈冰  李潇雨  罗丽萍
作者单位:1. 中国地质科学院矿产综合利用研究所,成都,610041
2. 成都理工大学沉积"油气藏地质及开发工程"国家重点实验室,成都,610059
3. 中国地质科学院矿产综合利用研究所,成都610041;成都理工大学沉积"油气藏地质及开发工程"国家重点实验室,成都610059
基金项目:科技部国际科技合作项目 
摘    要:四川会理拉拉铜矿床是我国著名大型富铜矿床,矿床的形成与古元古代河口群海相火山岩密切相关。河口群火山岩除个别样品Nb/Y较低,其他多数样品有一致高的Nb/Y比值(0.7~3.0),属碱性玄武系列;在Nb/Th-Zr/Nb和Zr/Y-Nb/Y图上,HFSE比值成分点主要投在EM1型富集地幔附近,落入洋岛玄武岩(OIB)范围;火山岩较陡的REE分布型式和"驼峰"状微量元素原始地幔标准化分配型式,以及缺乏Nb、Ta负异常,与大陆玄武岩十分吻合;岩石形成于板内裂谷环境。这些地球化学特征表明,河口群火山岩形成于陆间裂谷,来源于地幔深部,指示了矿床的火山喷流沉积成矿作用。同时,岩石大离子元素和轻稀土元素比值不太稳定,变化较大,Eu负异常与蚀变重晶石、萤石和矿化有关,还暗示了岩石遭受了后期变质作用,以及与之有关的矿床变质成矿成因。

关 键 词:铜矿床  含矿岩系  地球化学  构造意义  会理  四川

Geochemical and tectonic setting of the ore-bearing rock series occurred in the Lala copper deposit
ZHOU Jia-yun,ZHENG Rong-cai,ZHU Zhi-min,CHEN Jia-biao,SHEN Bing,LI Xiao-yu,LUO Li-ping.Geochemical and tectonic setting of the ore-bearing rock series occurred in the Lala copper deposit[J].Mineral Resources and Geology,2009,23(2).
Authors:ZHOU Jia-yun  ZHENG Rong-cai  ZHU Zhi-min  CHEN Jia-biao  SHEN Bing  LI Xiao-yu  LUO Li-ping
Institution:1 (1.Institute of Multipurpose Utilization of Mineral Resources; Chinese Academy of Geological Sciences; Chengdu 610041; China; 2.State Key Laboratory of Oil and Gas Reservoir and Exploitation; Chengdu University of Technology; Chengdu 610059; China);
Abstract:As a famous large-scale copper rich deposit in China,the Lala copper deposit in Huili of Sichuan Province is formed as a result of close influence brought by marine volcanic rocks of Palaeoproterozoic Hekou Group,which are characterized by high Nb/Y ratios(0.7~3.0) with minor rocks having relative low Nb/Y ratio,and can be concluded as alkali basalt rocks;on the diagrams of Nb/Th-Zr/Nb and Zr/Y-Nb/Y,HFSE values often fall in the neighborhood of EMI-enriched mantle within the range of OIB;the steep REE patte...
Keywords:Lala copper deposit  ore-bearing rock series  geochemistry  tectonic setting  Huili  Sichuan
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