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新疆哈密清白山铅锌矿矿床成因及成矿模型探讨
引用本文:夏天.新疆哈密清白山铅锌矿矿床成因及成矿模型探讨[J].新疆地质,2019(3):309-312.
作者姓名:夏天
作者单位:新疆维吾尔自治区地质调查院
摘    要:在总结清白山铅锌矿矿床地质特征、控矿因素的基础上,通过与MVT型矿床典型特征对比,认为其成因类型为MVT型。通过总结控矿因素,讨论了成矿时代,初步建立成矿模型,认为矿床成型分为含矿流体沉淀的主成矿期、构造改造期、岩浆改造期3个阶段。

关 键 词:地质特征  MVT型铅锌矿床  成矿时代  成矿模型

Discussion on Genesis and Metallogenic Model of Qingbaishan Lead-Zinc Deposit in Hami,Xinjiang
Xia Tian.Discussion on Genesis and Metallogenic Model of Qingbaishan Lead-Zinc Deposit in Hami,Xinjiang[J].Xinjiang Geology,2019(3):309-312.
Authors:Xia Tian
Affiliation:(Xinjiang geological suvey academy,Urumqi,Xinjiang,830000,China)
Abstract:Based on the summary of the geological characteristics and ore-controlling factors of the Qingbaishan lead- zinc deposit,the authors consider that the genetic type is MVT type by comparing with the typical characteristics of the MVT deposit.By summarizing the ore-controlling factors,the metallogenic age is discussed.The metallogenic model was established.It is believed that the formation of the deposit is divided into three stages:main ore-forming period,tectonic transformation period and magma transformation period.
Keywords:Geological characteristics  MVT-type lead-zinc deposit  Metallogenic age  Metallogenic model
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