引用本文:石洪召, 林方成, 张林奎.钨矿床的时空分布及研究现状[J].沉积与特提斯地质,2009,(4):90-95.[点击复制]
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钨矿床的时空分布及研究现状
石洪召,林方成,张林奎
0
(1. 中国地质科学院;
2. 成都地质矿产研究所)
摘要:
本文在查阅国内外钨矿资料的基础上,总结了钨矿床的时空分布、矿床类型、成因以及白钨矿在同位素测年方面的应用,阐述了钨矿床的成因研究现状及其发展趋势。
关键词:  钨矿床  时空分布  成因类型  白钨矿测年  研究现状
DOI:
附件
基金项目:“十一五”国家科技支撑计划项目“三江-湄公河成矿带地质背景和成矿规律对比研究”(2006BAB01A03-3);中国地质调查局“中缅边界三江西南段-掸邦成矿带成矿背景及成矿规律对比研究”(1212010913035);中国地质调查局“云南麻栗坡地区矿产远景调查”(1212010880402)
Spatio-temporal distribution and current state of the research of the tungsten deposits:An overview
SHI Hong-zhao, LIN Fang-cheng, ZHANG Lin-kui
(1. Chinese Academy of Geological Sciences, Beijing 100037, China;
2. Chengdu Institute of Geology and Mineral Resources, Chengdu 610082, Sichuan, China)
Abstract:
The present paper gives an overview of the spatio-temporal distribution,type,genesis,Sm-Nd dating of scheelite and current state of the research of the tungsten deposits.The tungsten deposits in the world are dominantly developed in the circum-Paific metallogenic zone,north of the Mediterranean Sea,South Ural,and Western and Central Asia.The mineralization ages span the Proterozoic to the Cenozoic,especially the Mesozoic.In China,tungsten mineralization occurred mostly during the early Yanshanian.The volcanic-sedimentary type is the main genetic type.
Key words:  tungsten deposit  spatio-temporal distribution  genetic types  Sm-Nd dating of scheelite  current state of research

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