| 北武夷陈坊铜多金属矿成矿地质特征与找矿方向 |
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| 引用本文： | 吴德来,;华荣辉,;李伯春.北武夷陈坊铜多金属矿成矿地质特征与找矿方向[J].火山地质与矿产,2008(4):279-288. |
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| 作者姓名： | 吴德来 ;华荣辉 ;李伯春 |
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| 作者单位： | [1]中国地质大学,湖北武汉430074; [2]江西省地质矿产勘查开发局赣东北大队,江西上饶334000 |
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| 基金项目： | 中国地质调查局“江西怀玉山-北武夷铜多金属矿评价”项目（1212010532901）资助. |
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| 摘 要： | 武夷山成矿带是我国重点成矿带之一，分布着众多的铜铅锌银等多金属矿床，矿床类型多样。本文在讨论陈坊铜多金属矿成矿地质特征的基础上，通过系统研究陈坊地区石炭纪地层中受接触带构造控制的矽卡岩型和二叠纪地层中主要为受层问破碎带控制的矽卡岩型铜铅锌多金属矿体的分布特征，探讨该区控矿因素、矿床成因分析，表明陈坊矿区成矿潜力巨大，并提出该区下一步找矿方向的建议。
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| 关 键 词： | 矽卡岩型 铜多金属矿 找矿方向 北武夷 陈坊 |
Metallogenetic geological characteristics and prospecting direction of Chenfang copper-polymetallic ore deposit in the northern Wuyishan mountain area |
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| Affiliation: | WU De-lai, HUA Rong-hui, LI Bo-chun ( 1 China University of Geoscience, Wuhan 430074, China;2 Northeastern Jiangxi Geoexploration team,Bureau of Geoexploration and Mineral resources, Shangrao 33400, China) |
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| Abstract: | The Wuyishan mountain metallogenetic belt is one of the important metallogenetic belts in China,where are distributed amounts of copper,lead, zinc and silver polymetallic deposits of multiple type. Based on analysing metallogenetic geological characteristics of the Chenfang copper-polymetallic deposit, this paper systematically studies the distribution features of skarn-type copper,lead and trolling factors and geneses of deposits. The result of the study indicates the great metallogenetic potentials of the Chenfang mineralizing area,therefore the ore-prospecting direction of the area in the next stage is suggested. |
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| Keywords: | skarn-type eopper-polymetallic ore deposit ore-prospecting direction northern Wuyishan mountain area Chenfang area |
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