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凡口超大型铅锌矿床成矿流体的物理特征和地球化学特征
引用本文:陈学明,邓军.凡口超大型铅锌矿床成矿流体的物理特征和地球化学特征[J].地球科学,2000,25(4):438-442.
作者姓名:陈学明  邓军
作者单位:中国地质大学地球科学与资源学院, 北京 100083
基金项目:国家攀登计划项目专题!( 95 -预 -3 9-2 -1),国土资源部“百名跨世纪科技人才培养计划”基金!( 980 8),国土资源部重大基础项目
摘    要:流体是汲取矿质、搬运矿质和沉淀矿质的介质, 是当代盆地研究和成矿研究的重要课题.在野外矿床地质研究和室内镜下研究、地球化学研究的基础上, 对矿区矿物流体包裹体的温度、盐度和化学成分的测试分析结果表明, 凡口矿床的成矿流体为低盐度、弱酸性的中低温热液, 属富CO2的K+-Ca2+-Cl-型的流体.它既不同于盆地压实流体, 也不同于斑岩型矿床的成矿流体, 是具有独特组成的深部循环流体 

关 键 词:超大型层控矿床    海底热泉    深部循环流体    广东凡口
文章编号:1000-2383(2000)04-0438-05
收稿时间:1999-08-31

GEOPHYSICAL AND GEOCHEMICAL FEATURES OF ORE-FORMING FLUID IN FANKOU SUPER-LARGE LEAD-ZINC DEPOSIT
Chen Xueming,Deng Jun,Shen Chonghui,Lan Jingzhi.GEOPHYSICAL AND GEOCHEMICAL FEATURES OF ORE-FORMING FLUID IN FANKOU SUPER-LARGE LEAD-ZINC DEPOSIT[J].Earth Science-Journal of China University of Geosciences,2000,25(4):438-442.
Authors:Chen Xueming  Deng Jun  Shen Chonghui  Lan Jingzhi
Affiliation:Chen Xueming ,Deng Jun ,Shen Chonghui ,Lan Jingzhi (Faculty of Earth Sciences and Mineral Resources, China University of Geosciences, Beijing 100083, China)
Abstract:The ore forming fluid, a medium that absorbs, transports and precipitates mineral materials, is an important topic for the research into the contemporary basin and mineralization. The testing analysis is made of the temperature, salinity and chemical composition of the mineral fluid inclusions in the deposit, on the basis of the field geological research into mineral deposits, the indoor microscopic research and geochemical research. The testing analytical results show that Fankou ore bearing fluid, the intermediate low temperature hydrothermal liquid low in salinity and weak in acidity, belongs to K + Ca 2+ Cl types of deep circulating ore bearing fluid rich in CO 2. This ore bearing fluid, a specific deep circulating fluid, differs not only from the basin compaction fluid but also from the ore forming fluid in the porphyrite type deposit.
Keywords:super  large stratabound deposit  submarine hot spring  deep  circulating fluid  Fankou of Guangdong Province  
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