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普朗大型斑岩铜矿控矿条件
引用本文:谭康华,李光军,黄定柱,张世全.普朗大型斑岩铜矿控矿条件[J].云南地质,2005,24(2):167-174.
作者姓名:谭康华  李光军  黄定柱  张世全
作者单位:云南省地质调查院矿产调查所,大理市,下关,671000
摘    要:普朗大型斑岩铜矿受区域地质、构造、地层、岩浆岩、岩体蚀变的综合控制,形成有其自身的特点和成矿条件。区域性断裂控制多期岩体侵入,形成普朗复式斑岩体;活动性差的硅铝质砂板岩形成岩体的天然屏障;不同期次构造交汇部位,形成密集的构造裂隙,为矿质的运移和积淀提供有利条件;多期多类型蚀变使矿质富集形成工业矿体。

关 键 词:大型斑岩铜矿  构造控制  岩浆岩侵入  蚀变富集  普朗香格里拉(中甸)
文章编号:1004-1885(2005)02-167-08

THE ORE-CONTROLLING CONDITIONS OF LARGE SCALE PULANG PORPHYRY COPPER DEPOSIT
TAN Kang-hua,LI Guang-jun,HUANG Ding-zhu,ZHANG Shi-quan.THE ORE-CONTROLLING CONDITIONS OF LARGE SCALE PULANG PORPHYRY COPPER DEPOSIT[J].Yunnan Geology,2005,24(2):167-174.
Authors:TAN Kang-hua  LI Guang-jun  HUANG Ding-zhu  ZHANG Shi-quan
Abstract:The large scale Pulang porphyry Cu deposit is comprehensively controlled by the regional geology, structure, stratigraphy, magmatic rocks and rockbody alteration, which has its genetic characteristics and metallogenetic conditions. The intrusions of multistage rockbody are controlled by the regional fault, which form the Pulang composite porphyry body. The inactive sialic sand-slate is a natural barrier. There are dense fissures formed in the intersection places of different stage structure, which provide the advantageous conditions for the moving and precipitation of ore material. And the multistage,polygeneous alterations cause the ore material to concentrate and form the industrial orebodies.
Keywords:Porphyry Cu Deposit  Structure  Magmatic Rock  Alteration  Pulang Xianggelila  
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