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鄂东南地区金井咀金矿早白垩世闪长岩Sr-Nd及锆石Hf同位素研究

李岩, 程春, 苏绍明, 高剑峰, 黄费新, 熊映志, 张岩, 黄华. 2023. 鄂东南地区金井咀金矿早白垩世闪长岩Sr-Nd及锆石Hf同位素研究[J]. 中国地质, 50(5): 1573-1585. doi: 10.12029/gc20200611002
引用本文: 李岩, 程春, 苏绍明, 高剑峰, 黄费新, 熊映志, 张岩, 黄华. 2023. 鄂东南地区金井咀金矿早白垩世闪长岩Sr-Nd及锆石Hf同位素研究[J]. 中国地质, 50(5): 1573-1585. doi: 10.12029/gc20200611002
LI Yan, CHENG Chun, SU Shaoming, GAO Jianfeng, HUANG Feixin, XIONG Yingzhi, ZHANG Yan, HUANG Hua. 2023. Sr-Nd and zircon Hf isotopic constraints on petrogenesis of the Early Cretaceous diorite in the Jinjingzui gold deposit, southeast Hubei Province[J]. Geology in China, 50(5): 1573-1585. doi: 10.12029/gc20200611002
Citation: LI Yan, CHENG Chun, SU Shaoming, GAO Jianfeng, HUANG Feixin, XIONG Yingzhi, ZHANG Yan, HUANG Hua. 2023. Sr-Nd and zircon Hf isotopic constraints on petrogenesis of the Early Cretaceous diorite in the Jinjingzui gold deposit, southeast Hubei Province[J]. Geology in China, 50(5): 1573-1585. doi: 10.12029/gc20200611002

鄂东南地区金井咀金矿早白垩世闪长岩Sr-Nd及锆石Hf同位素研究

  • 基金项目:
    国家重点研发计划(2016YFC0600207)和中国冶金地质总局矿产资源研究院自筹项目联合资助
详细信息
    作者简介: 李岩, 男, 1988年生, 高级工程师, 主要从事岩石学和矿床学研究; E-mail: liyan@cmgb.cn
    通讯作者: 程春, 男, 1969年生, 教授级高级工程师, 主要从事矿床学研究; E-mail: chengchun@cmgb.cn
  • 中图分类号: P588.12;P597.1

Sr-Nd and zircon Hf isotopic constraints on petrogenesis of the Early Cretaceous diorite in the Jinjingzui gold deposit, southeast Hubei Province

  • Fund Project: Supported by the National Key R&D Program of China (No.2016YFC0600207) and Science Foundation of Institute of Mineral Resources Research, China Metallurgical Geology Bureau
More Information
    Author Bio: LI Yan, male, born in 1988, senior engineer, mainly engaged in petrology and metallogeny survey; E-mail: liyan@cmgb.cn .
    Corresponding author: CHENG Chun, born in 1969, professor of engineering, mainly engaged in metallogeny survey; E-mail: chengchun@cmgb.cn
  • 研究目的

    金井咀金矿床早白垩世闪长岩的岩石成因及岩浆起源对于讨论成岩成矿关系、完善区域成矿规律等问题具有重要意义。

    研究方法

    本文对矿区赋矿闪长岩开展了全岩Sr-Nd和锆石Hf同位素分析。

    研究结果

    金井咀闪长岩具有相对较高的87Sr/86Sr初始比值(0.7059~0.7062),负的εNdt)值(-7.93~-7.58)和锆石εHft)值(-12.2~-6.5),表明岩浆形成于富集地幔的部分熔融,后经历了演化分异,在岩浆演化过程中可能存在一定程度的陆壳混染。

    结论

    通过与区域上已经发现的矿床对比发现,金井咀矽卡岩型金矿床与鄂东南矿集区矽卡岩型金矿床具有相同的成岩成矿时代和类似的岩石成因及岩浆源区,但是金井咀矿床金矿体主要赋存在闪长岩体内部,这与其他矿床主要赋存在碳酸盐岩地层或岩体内外接触带明显不同。金井咀矿床的发现,对于完善区域成矿规律,指导金矿找矿勘查具有重要的意义。

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  • 图 1  长江中下游成矿带地质矿产简图(据常印佛等,1991; Xie et al., 2011b

    Figure 1. 

    图 2  鄂东南矿集区主要岩体及矿床分布分图(据李新昊等,2018修改)

    Figure 2. 

    图 3  金井咀矿区地质图(a)及矿体剖面图(b)

    Figure 3. 

    图 4  金井咀矿床矿石及闪长岩手标本及镜下照片

    Figure 4. 

    图 5  金井咀矿床矿物生成序列图

    Figure 5. 

    图 6  金井咀闪长岩锆石阴极发光照片及测年结果

    Figure 6. 

    图 7  金井咀金矿闪长岩锆石U-Pb年龄谐和图

    Figure 7. 

    图 8  金井咀闪长岩(87Sr/86Sr)i-εNd(t)图(据Xie et al., 2011a

    Figure 8. 

    图 9  锆石Hf同位素特征图(底图引自Vervoort et al., 1996

    Figure 9. 

    表 1  金井咀闪长岩锆石U-Pb同位素组成

    Table 1.  Zircon U-Pb isotopic compositions of zircons in Jinjingzui diorite

    下载: 导出CSV

    表 2  金井咀闪长岩Sr-Nd同位素组成

    Table 2.  Sr-Nd isotopic compositions of Jingjingzui diorite

    下载: 导出CSV

    表 3  金井咀闪长岩锆石Hf同位素组成

    Table 3.  Zircon Hfisotopic composition of diorite in Jinjingzui

    下载: 导出CSV
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收稿日期:  2020-06-11
修回日期:  2020-08-25
刊出日期:  2023-10-25

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