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流水径矿区磁铁矿地质特征及成矿模式探讨
引用本文:钟才文.流水径矿区磁铁矿地质特征及成矿模式探讨[J].中国科技信息,2011(15):21-22.
作者姓名:钟才文
作者单位:广东省地质局七五六地质大队,广东,惠东,516300
摘    要:东源县黄村流水径矿区磁铁矿经普查工作查明其为品位较高的磁铁矿、中型的规模。该矿赋存于上三叠系小坪组砂页岩及粉砂岩等地层组成的近北东向平缓的小向斜构造中,本文认为其可能属陆相火山—侵入型铁矿床。该矿区的北东部小坪组地层中储量远景较大,可能找到品位更富、储量更大的磁铁矿体。

关 键 词:磁铁矿  流水径  地质特征  成矿模式  陆相火山—侵入型

Liushuijing Mining Area Magnetite Geological Feature And Mineralization Pattern Discussion
ZHONG Cai Wen.Liushuijing Mining Area Magnetite Geological Feature And Mineralization Pattern Discussion[J].CHINA SCIENCE AND TECHNOLOGY INFORMATION,2011(15):21-22.
Authors:ZHONG Cai Wen
Institution:ZHONG Cai Wen 756 Geologic Team of Bureau of Geology of Guangdong Province,Guangdong Huidong 516300
Abstract:The magnetite of Liushuijing mining area of huangcun in Dongyuan County verifies it after the coarse work for the high-grade magnetite and medium scale.This ore tax saves in the previous three packs is xiaoping ground stratum compositions and so on group sandy slate/shale and siltstone near north east to the gentle small syncline structure in,this article thought that it is possibly the land facies volcano-invasion profiled iron ore deposit.North of the mine in the eastern part of the xiaoping ground format...
Keywords:Magnetite  liushuijing  Geological feature  Mineralization pattern  Land facies volcano-invasion  
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