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云南新平县鱼塘铜矿床特征及成因浅析
引用本文:彭星宇,周宇,李仕斌.云南新平县鱼塘铜矿床特征及成因浅析[J].云南地质,2020(1):41-45.
作者姓名:彭星宇  周宇  李仕斌
作者单位:云南省有色地质局地质地球物理化学勘查院
摘    要:云南新平县鱼塘铜矿位于元谋-大红山铜成矿带南部,矿体呈似层状、透镜状产于古元古界大红山群肥味河组(Pt1 f)和曼岗河组(Pt1m)地层中,地层控矿明显。矿石以隐晶质结构、浸染状构造为主,矿床成因与“大红山铜矿”相似,属于海相火山沉积-变质铜矿床。

关 键 词:地层控矿  火山沉积-变质矿床  云南新平鱼塘

THE FEATURE AND A PRELIMINARY ANALYSIS OF GENESIS OF YUTANG CU DEPOSIT IN XINPING,YUNNAN
PENG Xing-yu,ZHOU Yu,LI Shi-bin.THE FEATURE AND A PRELIMINARY ANALYSIS OF GENESIS OF YUTANG CU DEPOSIT IN XINPING,YUNNAN[J].Yunnan Geology,2020(1):41-45.
Authors:PENG Xing-yu  ZHOU Yu  LI Shi-bin
Institution:(Exploration Institute of Geology,Geophysics-Geochemistry,Yunnan Bureau of Nonferrous Geology,Kunming 650011)
Abstract:Yutang Cu deposit in Xinping,Yunnan is in the S part of Yuanmou-Dahongshan Cu metallogenesis zone.The orebody is stratoid,lenticular in Paleo-Proterozoic Dahoangshan Group Feiweihe Formation(Pt1f)and Manganghe Formation(Pt1m),ore control of strata clear.The ore is mainly cryptocrystalline,disseminated.The deposit genesis is similar to that of“Dahoangshan Cu depost”,belonging to marine volcanic sedimentation-metamorphic Cu deposit.
Keywords:Ore Control of Strata  Volcanic Sedimentary-Metamorphic Deposit  Yutang  Xinping  Yunnan
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