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文山杨柳井铝土矿矿床成因及找矿标志
引用本文:缪鹰.文山杨柳井铝土矿矿床成因及找矿标志[J].云南地质,2009,28(3):291-294.
作者姓名:缪鹰
作者单位:云南地质矿产勘查院大理地质矿产所,大理,67100
摘    要:铝土矿产于第四系残坡积层中,属堆积型,分布于大塘组及威宁组形成的溶蚀漏斗及洼地中。讨论矿床成因及找矿标志。

关 键 词:堆积型铝土矿床  成矿控制因素  矿化富集规律  找矿标志  云南文山铝土矿

THE GENESIS AND PROSPECTING CRITERIA OF THE BAUXITE DEPOSIT IN WENSHAN
MIAO Ying.THE GENESIS AND PROSPECTING CRITERIA OF THE BAUXITE DEPOSIT IN WENSHAN[J].Yunnan Geology,2009,28(3):291-294.
Authors:MIAO Ying
Institution:MIAO Ying (Dali Branch, Yunnan Exploraion Institute of Geology & Mineral Resources, Dali 671000)
Abstract:The bauxite deposit is in Quaternary eluvium -slop wash, accumulation type. The ore - bearing eluvium - slop wash is in the karst funnel and depression formed in Carboniferous Datang Formation and Weining Formation. The genesis and prospecting criteria of it are interpreted in this paper.
Keywords:Bauxite Deposit of Accumulation Type  Control Factors of MetaUogenesis  Concentration Law of Metallogenesis  Prospecting Criteria  Wenshan Bauxite Deposit  Yunnan
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