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云南哀牢山金矿带北西段地质特征与找矿靶区

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云南哀牢山金矿带北西段牛街地区三条金矿化蚀变带矿体呈层状赋存于下古生界绢云石英微晶片岩构造破碎带中,总体呈北西-南东向展布,倾向北东,厚度 0.69m~4.11m,Au品位 1.10ω×10-6~4.20ω×10-6,矿床成因为浅变质碎屑岩型.构造破碎带、富矿层位、侵入岩体及硅化-褐铁矿化(黄铁矿化)带同时有物、化探异常叠合部位是寻找金矿有利地段,圈定了三个找矿靶区.
GEOLOGICAL CHARACTERISTICS AND PROSPECTING TARGETS OF THE NORTHWEST SECTION OF THE AILAOSHAN GOLD BELT,YUNNAN
Ore bodies of the three gold mineralization alteration zones in the Niujie area,northwesternAilaoshan gold belt,Yunnan,are layered in thestrutuaral fracture zone of the Lower Paleozoic sericite quartz microcrystalline schist.They are generally distributed in the NW-SE direction,inclined toNE,with a thickness of 0.69-4.11m and an Au grade of 1.10ω×10-6~4.20ω×10-6.The deposit is of low metamorphic clastic rock type.The structural fracture zones,the ore-rich layers,the intrusive rock masses and the silicification-limonite(pyrite)mineralization zones with both physical and geochemical anomalies are the favorable areas for exploring gold deposits.Three prospecting target areas have been delineated.

Stratigraphy and Structural Ore ControlIntrusive RocksProspecting Target AreaAilaoshan Gold Mineralization BeltMidu,Yunnan

文加春、孙技星

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云南省地质科学研究所,云南 昆明 650051

地层+构造控矿 侵入岩体 找矿靶区 哀牢山金矿带 云南弥渡

2024

云南地质
云南省地矿总公司 云南省地质矿产勘查院

云南地质

影响因子:0.259
ISSN:1004-1885
年,卷(期):2024.43(3)