节点文献

兰坪金顶大规模成矿的流体过程——不同矿化阶段流体包裹体微量元素约束

Fluid processes of a heavy metallogenesis at Jinding,Lanping,SW-China.

  • 推荐 CAJ下载
  • PDF下载
  • 不支持迅雷等下载工具,请取消加速工具后下载。

【作者】 薛春纪曾荣高永宝朱和平赵世华李永强

【Author】 XUE ChunJi~1 ZENG Rong~2 GAO YongBao~2 ZHU HePing~3 ZHAO ShiHua~2 LI YongQiang~2 1.State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Beijing 100083,China 2.Faculty of Earth Sciences and Land Resource,Chang’an University,Xi’an 710054,China 3.Institute of Geology and Geophysics,China Academy of Sciences,Beijing 100029,China

【机构】 中国地质大学(北京)地质过程与矿产资源国家重点实验室地学院长安大学地球科学与国土资源学院中国科学院地质与地球物理研究所长安大学地球科学与国土资源学院 北京100083西安710054北京100029

【摘要】 金顶矿床是世界上形成时代最新且唯一的陆相沉积岩容矿的超大型铅锌矿床,受人关注。金顶矿石中矿物的交生关系表明内生流体成矿经历了石英-闪锌矿-方铅矿、闪锌矿-方铅矿-天青石、方铅矿-方解石-天青石-石膏三个矿化阶段,黄铁矿在各矿化阶段中均有形成,不同世代矿物从产状、结构、组合关系等得以区分;矿物流体包裹体中包括REE在内的几十种微量元素的配分曲线和含量分布不因寄主矿物种类而明显变化,不同矿化阶段矿物流体包裹体微量元素组成是大规模成矿流体过程的重要约束;大规模成矿从第1到第3矿化阶段,内生成矿流体∑REE逐步升高(1.34×10-9~6.28×10-9~297.03×10-9),轻重REE分异越趋显著,系统从还原性演化为氧化性,微量元素组合趋于复杂,流体中成矿元素(Zn 13.594×10-9~29331.810×10-9)不断富集(Zn依次是中国陆壳的0.16×10-3~0.20×10-3倍、0.041~0.193倍、0.028~0.341倍);早—中阶段的流体成矿可能是快速的,中—晚阶段趋缓;深、浅部两种不同性质流体混合可能是流体大规模成矿的基本过程。

【Abstract】 The Jinding ore deposit is the youngest and the only giant deposit hosted in continental sedimentary rocks in the world,and followed with interests.The Jinding fluid mineralization experienced three stages,they are quartz-sphalerite-galena,sphalerite-galena- celestite and galena-calcite-celestite-gypsum,according to the intergrowth of minerals in the Jinding ores.Pyrite occurs in each stage, and various generations of minerals can be distinguished by their occurrence,texture and assemblage relations.Rare element compositions in fluid inclusions are an important indicator of the large-scale fluid metallogenic processes because the REE patterns and rare element distributions of the fluid inclusions in minerals of various mineralization stages do not evidently change in different hosted minerals.From the first to the third mineralization stage of the fluid mineralization processes,∑REE(1.34×10-9~6.28×10-9~297.03×10-9)and LREE/HREE increased in the ore-forming fluid respectively,and the fluid system became more oxidizing,the rare element assemblage of the ore-forming fluid became more complex,the metallogenic element(zinc changing from 13.594×10-9 to 29331.810×10-9)was richer and richer(zinc being 0.16×10-3~0.20×10-3 times,0.041~0.193 times and 0.028~0.341 times of China continental crust) in the ore-forming fluid.The fluid mineralization may be quick during the early-middle stage and slower during the middle-late stage. A mixing of a deep- and a shallow- fluid may be the essentials for the large-scale mineralization in the Jinding.

【基金】 国家重点基础研究发展规划(2002CB4126007);国家自然科学基金(40272050、40472054);长安大学科技发展基金(0303-1001)资助.
  • 【文献出处】 岩石学报 ,Acta Petrologica Sinica , 编辑部邮箱 ,2006年04期
  • 【分类号】P618.63
  • 【被引频次】41
  • 【下载频次】727
节点文献中: 

本文链接的文献网络图示:

本文的引文网络