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鲁西莱芜三岔河矽卡岩型铁金矿床岩体成因:锆石U-Pb年代学和岩石地球化学证据

马明, 高明波, 祝德成, 李亚东, 高继雷, 范振华, 冯启伟, 李思远, 张永明. 2022. 鲁西莱芜三岔河矽卡岩型铁金矿床岩体成因:锆石U-Pb年代学和岩石地球化学证据[J]. 中国地质, 49(6): 1893-1907. doi: 10.12029/gc20220614
引用本文: 马明, 高明波, 祝德成, 李亚东, 高继雷, 范振华, 冯启伟, 李思远, 张永明. 2022. 鲁西莱芜三岔河矽卡岩型铁金矿床岩体成因:锆石U-Pb年代学和岩石地球化学证据[J]. 中国地质, 49(6): 1893-1907. doi: 10.12029/gc20220614
MA Ming, GAO Mingbo, ZHU Decheng, LI Yadong, GAO Jilei, FAN Zhenhua, FENG Qiwei, LI Siyuan, ZHANG Yongming. 2022. Petrogenesis of the Sanchahe skarn type iron-gold deposit in Laiwu area, western Shandong: Evidences from zircon U-Pb geochronology and geochemistry[J]. Geology in China, 49(6): 1893-1907. doi: 10.12029/gc20220614
Citation: MA Ming, GAO Mingbo, ZHU Decheng, LI Yadong, GAO Jilei, FAN Zhenhua, FENG Qiwei, LI Siyuan, ZHANG Yongming. 2022. Petrogenesis of the Sanchahe skarn type iron-gold deposit in Laiwu area, western Shandong: Evidences from zircon U-Pb geochronology and geochemistry[J]. Geology in China, 49(6): 1893-1907. doi: 10.12029/gc20220614

鲁西莱芜三岔河矽卡岩型铁金矿床岩体成因:锆石U-Pb年代学和岩石地球化学证据

  • 基金项目:
    山东省第一地质矿产勘查院基金项目“鲁西莱芜三岔河矽卡岩型铁金矿床成矿作用及找矿方向研究”(KC202205)资助
详细信息
    作者简介: 马明, 男, 1989年生, 工程师, 主要从事地质调查与矿产勘查工作; E-mail: 928655084@qq.com
    通讯作者: 高明波, 男, 1978年生, 研究员, 主要从事岩石学、地球化学研究工作; E-mail: jngmb@126.com
  • 中图分类号: P597.3;P618.31;P618.51

Petrogenesis of the Sanchahe skarn type iron-gold deposit in Laiwu area, western Shandong: Evidences from zircon U-Pb geochronology and geochemistry

  • Fund Project: Supported by the fund of No.1 Institute of Geology and Mineral Resources of Shandong Province (No.KC202205)
More Information
    Author Bio: MA Ming, male, born in 1989, engineer, majors in geological survey and mineral exploration; E-mail: 928655084@qq.com .
    Corresponding author: GAO Mingbo, male, born in 1978, researcher, majors in the research of petrology and geochemistry; E-mail: jngmb@126.com
  • 研究目的

    莱芜三岔河矿床是鲁西地区首次发现的矽卡岩型铁金矿床(不含铜),以往研究相对薄弱,本文旨在对成矿岩体形成时代、源区性质、岩石成因和构造背景进行讨论。

    研究方法

    本文开展了LA-ICP-MS锆石U-Pb测年、岩体主微量测试工作。

    研究结果

    结果显示辉石闪长岩侵位年龄为(138.4±1.2)Ma,属早白垩世。辉石闪长岩里特曼指数σ=2.20~2.54,为钙碱性岩石;辉石闪长岩具高Mg#、富Na特征,Sc、Cr、Co、Ni含量较高,表明其具有幔源岩浆的属性;富集轻稀土元素(LREE),亏损重稀土元素(HREE),Eu异常不明显,富集大离子亲石元素(Cs、Ba、Sr),亏损高场强元素(Nb、Ta、Zr),暗示有地壳物质的涉入。

    研究结论

    三岔河辉石闪长岩可能起源于受华北克拉通古老地壳物质改造的富集岩石圈地幔的部分熔融,形成于岩石圈减薄的强烈伸展构造背景,可能与太平洋板块俯冲后撤引起的伸展构造环境有关。

  • 加载中
  • 图 1  华北克拉通地质简图(a)和鲁西地块地质简图(b)(a据Zhang et al., 2005;b据Lan et al., 2011修改)

    Figure 1. 

    图 2  三岔河矿区地质简图

    Figure 2. 

    图 3  三岔河矿区5勘查线地质剖面图

    Figure 3. 

    图 4  三岔河辉石闪长岩岩心照片(a)和显微镜下照片(b)

    Figure 4. 

    图 5  三岔河辉石闪长岩锆石阴极发光图像

    Figure 5. 

    图 6  三岔河辉石闪长岩锆石LA-ICP-MS U-Pb年龄谐和图

    Figure 6. 

    图 7  三岔河辉石闪长岩硅碱图解(a)和SiO2-K2O图解(b)

    Figure 7. 

    图 8  三岔河辉石闪长岩稀土元素球粒陨石标准化配分图(a)和微量元素地幔标准化蛛网图(b)

    Figure 8. 

    表 1  三岔河辉石闪长岩LA-ICP-MS锆石U-Pb同位素分析结果

    Table 1.  Analyzed results of LA-ICP-MS zircons U-Pb of the Sanchahe pyroxene diorite

    下载: 导出CSV

    表 2  三岔河辉石闪长岩主量元素(%)、微量和稀土元素(10-6)化学分析结果

    Table 2.  Chemical compositions of major elements, trace elements and REE elements of the Sanchahe pyroxene diorite

    下载: 导出CSV
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出版历程
收稿日期:  2020-04-16
修回日期:  2020-11-12
刊出日期:  2022-12-25

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