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黑龙江省东北部多宝山地区中奥陶世侵入岩锆石U-Pb年龄及构造环境

于喜洹 石国明 符安宗 李新鹏 孙江军 尹国良 林泽付

于喜洹, 石国明, 符安宗, 李新鹏, 孙江军, 尹国良, 林泽付. 黑龙江省东北部多宝山地区中奥陶世侵入岩锆石U-Pb年龄及构造环境[J]. 仁和测试. doi: 10.13686/j.cnki.dzyzy.2022.05.002
引用本文: 于喜洹, 石国明, 符安宗, 李新鹏, 孙江军, 尹国良, 林泽付. 黑龙江省东北部多宝山地区中奥陶世侵入岩锆石U-Pb年龄及构造环境[J]. 仁和测试. doi: 10.13686/j.cnki.dzyzy.2022.05.002
YU Xi-huan, SHI Guo-ming, FU An-zong, LI Xin-peng, SUN Jiang-jun, YIN Guo-liang, LIN Ze-fu. ZIRCON U-PB AGE AND TECTONIC SETTING OF THE MIDDLE ORDOVICIAN INTRUSIVE ROCKS IN DUOBAOSHAN AREA, HEILONGJIANG PROVINCE[J]. Rhhz Test. doi: 10.13686/j.cnki.dzyzy.2022.05.002
Citation: YU Xi-huan, SHI Guo-ming, FU An-zong, LI Xin-peng, SUN Jiang-jun, YIN Guo-liang, LIN Ze-fu. ZIRCON U-PB AGE AND TECTONIC SETTING OF THE MIDDLE ORDOVICIAN INTRUSIVE ROCKS IN DUOBAOSHAN AREA, HEILONGJIANG PROVINCE[J]. Rhhz Test. doi: 10.13686/j.cnki.dzyzy.2022.05.002

黑龙江省东北部多宝山地区中奥陶世侵入岩锆石U-Pb年龄及构造环境

doi: 10.13686/j.cnki.dzyzy.2022.05.002
基金项目: 

中国地质调查局“大兴安岭成矿带漠河-扎兰屯地区地质矿产调查”项目(DD20160047-07)

详细信息
    作者简介:

    于喜洹(1972—),男,高级工程师,从事区域地质调查及地质矿产勘查工作,通信地址黑龙江省哈尔滨市香坊区新乡里街9号,E-mail//278053757@qq.com

    通讯作者:

    石国明(1986—),男,高级工程师,从事区域地质调查工作,通信地址黑龙江省哈尔滨市香坊区新乡里街9号,E-mail//5142052@qq.com

  • 中图分类号: P597.1

ZIRCON U-PB AGE AND TECTONIC SETTING OF THE MIDDLE ORDOVICIAN INTRUSIVE ROCKS IN DUOBAOSHAN AREA, HEILONGJIANG PROVINCE

  • 摘要: 多宝山地区位于兴蒙造山带东段扎兰屯-多宝山岛弧构造带,早古生代地质体发育,且与区域成矿作用关系密切. 通过对多宝山地区中奥陶世侵入岩的岩相学、岩石地球化学、同位素年代学特征的研究,对其形成时代、构造环境及成矿作用进行了探讨. 定年结果显示花岗闪长岩LA-MC-ICP-MS锆石U-Pb年龄为488±3 Ma,形成时代为中奥陶世;岩浆物质来源以幔源为主,同熔了部分壳源物质,伴随强烈的构造热事件和岩浆侵入喷发活动,大量深源流体带来Au、Cu等成矿元素,在有利成矿条件和扩容空间下,形成多宝山铜(钼)矿床. 研究显示,中奥陶世花岗闪长岩形成于与板块俯冲有关的岛弧环境.

     

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出版历程
  • 收稿日期:  2021-06-02
  • 修回日期:  2021-07-12
  • 网络出版日期:  2022-11-09

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