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鄂东南付家山矽卡岩型(Cu-)W矿床成岩成矿时代及地质意义

刘泉 李艳军 蔡恒安 李红梅 曾小华 孙孝峰 刘冬勤 谭俊

刘泉, 李艳军, 蔡恒安, 李红梅, 曾小华, 孙孝峰, 刘冬勤, 谭俊. 鄂东南付家山矽卡岩型(Cu-)W矿床成岩成矿时代及地质意义[J]. 地质科技通报, 2021, 40(5): 210-222. doi: 10.19509/j.cnki.dzkq.2021.0042
引用本文: 刘泉, 李艳军, 蔡恒安, 李红梅, 曾小华, 孙孝峰, 刘冬勤, 谭俊. 鄂东南付家山矽卡岩型(Cu-)W矿床成岩成矿时代及地质意义[J]. 地质科技通报, 2021, 40(5): 210-222. doi: 10.19509/j.cnki.dzkq.2021.0042
Liu Quan, Li Yanjun, Cai Heng'an, Li Hongmei, Zeng Xiaohua, Sun Xiaofeng, Liu Dongqin, Tan Jun. Diagenetic and metallogenic ages, and geological significance of the Fujiashan skarn-type(Cu-) W Deposit, southeastern Hubei Province[J]. Bulletin of Geological Science and Technology, 2021, 40(5): 210-222. doi: 10.19509/j.cnki.dzkq.2021.0042
Citation: Liu Quan, Li Yanjun, Cai Heng'an, Li Hongmei, Zeng Xiaohua, Sun Xiaofeng, Liu Dongqin, Tan Jun. Diagenetic and metallogenic ages, and geological significance of the Fujiashan skarn-type(Cu-) W Deposit, southeastern Hubei Province[J]. Bulletin of Geological Science and Technology, 2021, 40(5): 210-222. doi: 10.19509/j.cnki.dzkq.2021.0042

鄂东南付家山矽卡岩型(Cu-)W矿床成岩成矿时代及地质意义

doi: 10.19509/j.cnki.dzkq.2021.0042
基金项目: 

中国地质大学(武汉)中央高校基本科研业务费"地学长江计划"核心项目群资助项目 CUGCJ1817

国家自然科学基金项目 41672083

湖北省地质局科技项目 KJ2021-9

中国矿产地质志项目 DD20190379

中国矿产地质志项目 DD20160346

湖北省地质勘查基金项目 〔2019〕1号

详细信息
    作者简介:

    刘泉(1994-), 男, 现正攻读地质工程专业硕士学位, 主要从事矿产勘查与评价研究工作。E-mail: 16637617216@163.com

    通讯作者:

    李艳军(1982-), 男, 副教授, 主要从事矿床地球化学、成矿规律与成矿预测教学和研究工作。E-mail: liyj@cug.edu.cn

    李红梅(1970-), 女, 教授级高级工程师, 主要从事地质矿产勘查及成矿规律研究工作。E-mail: 541083407@qq.com

  • 中图分类号: P618.2

Diagenetic and metallogenic ages, and geological significance of the Fujiashan skarn-type(Cu-) W Deposit, southeastern Hubei Province

  • 摘要: 付家山(Cu-)W矿床是鄂东南地区新近发现的大型矽卡岩型矿床之一,成矿与花岗闪长斑岩关系密切。为了精确获得该矿床成岩成矿年龄,利用LA-ICP-MS锆石U-Pb和辉钼矿Re-Os同位素定年法对其进行了系统的成岩成矿年代学研究,并基于长江中下游成矿带晚中生代沉积地层及构造变形、地球物理和岩石地球化学等证据探讨了其成岩成矿构造背景。结果显示:花岗闪长斑岩锆石U-Pb加权平均年龄为(144±3)Ma,而辉钼矿Re-Os模式年龄为(146±2)Ma,成岩与成矿作用均形成于晚侏罗世-早白垩世。付家山(Cu-)W矿床形成时代与长江中下游地区大规模岩浆成矿事件时间一致,包括鄂东南地区在内的长江中下游地区的构造演化历史及最新的年代学数据表明,付家山(Cu-)W矿床极有可能形成于岩石圈伸展减薄构造背景。付家山等晚侏罗世-早白垩世矽卡岩型(Cu-)W矿床的发现及厘定指示了鄂东南矿集区具有良好的钨矿找矿前景。

     

  • 图 1  鄂东南矿集区典型岩体及矽卡岩型矿床分布图(据文献[21]修改)

    Figure 1.  Distribution map of magmatism and skarn-type deposits in the southeastern Hubei Province

    图 2  付家山(Cu-)W矿床地质简图(据文献[12]修改)

    Figure 2.  Geological map of the Fujiashan (Cu-)W deposit

    图 3  付家山(Cu-)W矿床西侧矿区1011线(a)和东侧矿区17线(b)地质剖面图(据文献[13])

    Figure 3.  Geological profiles of Line 1011(a) in the western section and Line 17(b) in the eastern section of the Fujiashan(Cu-)W district

    图 4  付家山花岗闪长斑岩体镜下鉴定特征(均为正交偏光)

    Pl.斜长石;Kfs.钾长石;Q.石英; Hb.角闪石

    Figure 4.  Microscopic identification of the Fujiashan granodiorite porphyry

    图 5  付家山(Cu-)W矿床典型矿石结构

    a.闪锌矿交代黄铁矿;b.黄铜矿交代闪锌矿和黄铁矿;c.斑铜矿交代闪锌矿;d.白钨矿被闪锌矿包裹;e.辉钼矿被闪锌矿交代;f.白钨矿与绿泥石充填于石榴石间隙。Py.黄铁矿; Sp.闪锌矿; Cpy.黄铜矿; Bn.斑铜矿; Sch.白钨矿; Mol.辉钼矿; Grt.石榴石; Cal.方解石; Chl.绿泥石

    Figure 5.  Typical ores structure of Fujiashan (Cu-)W deposit

    图 6  付家山(Cu-)W矿床成矿阶段划分图

    Figure 6.  Mineralization stage of the Fujiashan (Cu-)W deposit

    图 7  鄂东南地区付家山花岗闪长斑岩(FJS-26)锆石U-Pb年龄谐和图

    Figure 7.  Zircon U-Pb ages of the Fujiashan granodiorite porphyry(FJS-26) in southeastern Hubei Province

    图 8  鄂东南付家山花岗闪长斑岩和其他类型花岗岩构造环境判别图(数据引自文献[11, 64-65])

    VAG.火山弧花岗岩; WPG.板内花岗岩; ORG.洋脊花岗岩; syn-COLG.同碰撞花岗岩; Post-COLG.后碰撞花岗岩

    Figure 8.  Tectonic discrimination diagram of the Fujiashan granodiorite porphyry and other typical granites in the south eastern Hubei Province

    表  1  付家山花岗闪长斑岩(FJS-26)LA-ICP-MS锆石U-Pb同位素数据

    Table  1.   LA-ICP-MS zircon U-Pb isotopic data of the Fujiashan granodiorite porphyry(sample FJS-26)

    分析点号 元素wB/10-6 Th/U 同位素比值 年龄/Ma
    Th U 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ
    FJS-26-01 225.2 445.1 0.51 0.051 9 0.003 3 0.153 7 0.009 8 0.021 6 0.000 5 283 153 145 9 138 3
    FJS-26-03 1 022.6 838.6 1.22 0.052 6 0.002 0 0.162 6 0.006 2 0.022 3 0.000 3 322 81 153 5 142 2
    FJS-26-05 413.6 479.3 0.86 0.056 2 0.002 4 0.179 0 0.007 5 0.023 2 0.000 3 461 94 167 6 148 2
    FJS-26-06 469.3 620.6 0.76 0.047 8 0.001 7 0.146 6 0.005 2 0.022 2 0.000 3 100 -114 139 5 141 2
    FJS-26-07 254.7 384.1 0.66 0.047 9 0.003 2 0.159 6 0.010 7 0.024 0 0.000 4 98 152 150 9 153 2
    FJS-26-08 238.7 319.5 0.75 0.048 8 0.002 2 0.154 6 0.006 5 0.023 2 0.000 3 200 104 146 6 148 2
    FJS-26-09 246.4 381.6 0.65 0.046 6 0.002 3 0.147 8 0.007 0 0.023 2 0.000 3 32 111 140 6 148 2
    FJS-26-10 869.0 657.8 1.32 0.050 5 0.002 1 0.152 0 0.006 1 0.021 9 0.000 3 220 101 144 5 140 2
    FJS-26-11 156.3 238.4 0.66 0.052 8 0.003 3 0.173 1 0.010 8 0.023 8 0.000 4 317 141 162 9 152 3
    FJS-26-12 1 039.4 749.6 1.39 0.048 3 0.001 8 0.147 1 0.005 5 0.022 1 0.000 3 117 89 139 5 141 2
    FJS-26-13 303.1 240.4 1.26 0.051 1 0.003 1 0.163 6 0.008 8 0.023 6 0.000 4 256 137 154 8 150 2
    FJS-26-14 473.0 529.1 0.89 0.050 1 0.002 0 0.162 1 0.006 6 0.023 4 0.000 3 198 99 153 6 149 2
    FJS-26-15 390.1 513.7 0.76 0.050 5 0.002 1 0.157 2 0.006 3 0.022 6 0.000 3 217 94 148 6 144 2
    FJS-26-16 590.7 831.7 0.71 0.049 1 0.001 7 0.145 4 0.005 0 0.021 5 0.000 3 150 77 138 4 137 2
    FJS-26-18 515.0 657.6 0.78 0.048 8 0.001 7 0.152 4 0.005 6 0.022 6 0.000 3 200 85 144 5 144 2
    FJS-26-19 689.9 659.9 1.05 0.050 3 0.001 9 0.148 8 0.005 7 0.021 4 0.000 2 209 90 141 5 136 2
    FJS-26-20 307.9 357.1 0.86 0.049 2 0.002 5 0.162 1 0.008 2 0.024 1 0.000 4 167 120 153 7 154 3
    下载: 导出CSV

    表  2  付家山(Cu-)W矿床辉钼矿Re-Os同位素组成

    Table  2.   Re-Os isotopic composition of Molybdenite from the Fujiashan(Cu-)W deposit

    样品编号 质量/g w(Re)/10-6 w(Os)/ 10-6 w(187Re)/10-6 w(187Os)/10-6 模式年龄t/Ma
    FJS-31 0.002 06 267.5±2.4 5.151±0.162 168.1±1.5 409.1±2.4 146±2
    下载: 导出CSV

    表  3  鄂东南地区典型矽卡岩型矿床成岩成矿年龄统计

    Table  3.   Statistics of diagenetic and metallogenic ages of typical skarn deposits in southeastern Hubei Province

    岩体名称 岩石名称 成岩时代/Ma 测试对象 成矿或蚀变年龄/Ma 测试方法 资料来源
    付家山 花岗闪长斑岩 144±3 LA-ICP-MS锆石U-Pb 本文
    矿体 146±2 辉钼矿Re-Os
    龙角山 花岗闪长斑岩 144±1 LA-ICP-MS锆石U-Pb 文献[11]
    矿体 144.7±2.9 辉钼矿Re-Os
    鸡冠咀 石英正长闪长玢岩 146±2 SHRIMP U-Pb 文献[37]
    闪长岩 132±4 SHRIMP U-Pb
    矿体 138.2±2.2 辉钼矿Re-Os 文献[19]
    蚀变岩 140.3±1.1 金云母40Ar/39Ar
    桃花咀 矿体 138.3±2 辉钼矿Re-Os 文献[19]
    矽卡岩 139.9±1.1 金云母40Ar/39Ar
    铜绿山 石英正长闪长玢岩 146±1 SHRIMP U-Pb 文献[38]
    石英闪长岩 140±2 SHRIMP U-Pb 文献[19]
    矿体 137.8±1.7 辉钼矿Re-Os 文献[15]
    矿体 138.1±1.8 辉钼矿Re-Os
    矿体 137.3±2.4 辉钼矿Re-Os 文献[19]
    矽卡岩 136.0±1.3 LA-ICP-MS榍石U-Pb 文献[35]
    姜桥 花岗闪长岩 144±1 LA-ICP-MS锆石U-Pb 文献[39]
    铜山口 花岗闪长岩 140.6±2.4 SHRIMP U-Pb 文献[30]
    矿体 143.8±2.6 辉钼矿Re-Os
    阮家湾 花岗闪长岩 143±1 SHRIMP U-Pb 文献[40]
    矿体 143.6±1.7 辉钼矿Re-Os 文献[15]
    犀牛山 花岗闪长斑岩 147±1 SHRIMP U-Pb 文献[40]
    丰山 花岗闪长斑岩 137±2 SHRIMP U-Pb 文献[37]
    矿体 144±2.1 辉钼矿Re-Os 文献[15]
    鸡笼山 花岗闪长斑岩 138±2 SHRIMP U-Pb 文献[37]
    岩体 151.8±0.7 锆石U-Pb 文献[41]
    矿体 150.7±0.8 辉钼矿Re-Os
    下载: 导出CSV
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  • 收稿日期:  2020-11-20

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