| 香格里拉陆家村银金多金属矿矿化特征及找矿标志 |
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| 引用本文： | 黄琴辉.香格里拉陆家村银金多金属矿矿化特征及找矿标志[J].云南地质,2010,29(4):499-502. |
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| 作者姓名： | 黄琴辉 |
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| 作者单位： | 昆明理工大学国土资源工程学院,昆明650093 |
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| 摘 要： | 研究区浅部以断裂破碎带控制的热液脉型Cu、Au、Pb、Ag矿床为主,深部形成斑岩型Cu、Mo矿床。矿体受地层及断裂构造双重控制。硅化、黄(褐)铁矿化与矿化关系最为密切,是主要的围岩蚀变,亦为主要的找矿标志。
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| 关 键 词： | 银金多金属矿床 热液脉型 成矿地质特征 找矿标志 香格里拉陆家村 |
THE METALLOGENETIC CHARACTERISTICS AND ORE PROSPECTING MARKS OF LUJIACUN AG-AU MULTIMETALLIC DEPOSIT,XIANGGELILA |
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| HUANG Hui-qin.THE METALLOGENETIC CHARACTERISTICS AND ORE PROSPECTING MARKS OF LUJIACUN AG-AU MULTIMETALLIC DEPOSIT,XIANGGELILA[J].Yunnan Geology,2010,29(4):499-502. |
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| Authors: | HUANG Hui-qin |
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| Institution: | HUANG Hui-qin ( College of Land Resource Engineering, Kunming University of Science ＆ Technology, Kunming 650093 ) |
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| Abstract: | In the shallow part of study area, the ore deposit is mainly the hydrothermal Ca, Au, Pb, Ag veined deposit controlled by fault zone, whereas the porphyry Cu, Mo deposit in the deep part. The ore bodies are controlled dually by strata and fault structure. The silisification, pyritization （limonitization） are in elose relation with the metallogenesis, which are the main alteration of wall rock and the main marks in ore prospecting. |
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| Keywords: | Ag - Au Multimetallic Deposit Hydrothermal Vein Type Metallogenefic Geological Characteristics Ore Prospecting Marks Lujiacun Xianggelila |
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