敖光. 张广才岭南部侵入岩锆石U-Pb LA-ICP-MS年代[J]. 地质与资源, 2016, 25(6): 533-538. DOI: 10.13686/j.cnki.dzyzy.2016.06.004
    引用本文: 敖光. 张广才岭南部侵入岩锆石U-Pb LA-ICP-MS年代[J]. 地质与资源, 2016, 25(6): 533-538. DOI: 10.13686/j.cnki.dzyzy.2016.06.004
    AO Guang. ZIRCON U-Pb LA-ICP-MA AGE OF THE INTRUSIVE ROCK IN SOUTHERN ZHANGGUANGCAILING AREA[J]. Geology and Resources, 2016, 25(6): 533-538. DOI: 10.13686/j.cnki.dzyzy.2016.06.004
    Citation: AO Guang. ZIRCON U-Pb LA-ICP-MA AGE OF THE INTRUSIVE ROCK IN SOUTHERN ZHANGGUANGCAILING AREA[J]. Geology and Resources, 2016, 25(6): 533-538. DOI: 10.13686/j.cnki.dzyzy.2016.06.004

    张广才岭南部侵入岩锆石U-Pb LA-ICP-MS年代

    ZIRCON U-Pb LA-ICP-MA AGE OF THE INTRUSIVE ROCK IN SOUTHERN ZHANGGUANGCAILING AREA

    • 摘要: 张广才岭是中生代花岗质岩浆作用较为发育的地区,但关于该地区花岗岩的形成时代,缺少精确的同位素年龄资料.本文通过“黑龙江1:5万大贯屯(L52E023007)等四幅区域地质矿产调查”项目,对工作区内的花岗质岩进行了锆石U-Pb同位素测年,结果显示:三叠纪花岗岩形成于224~229 Ma,侏罗纪侵入岩形成于202~193 Ma.

       

      Abstract: Mesozoic granitic magmatism is developed in the Zhangguangcaling area. However, accurate isotopic age data is lack for the granite in the area. Based on the 1:50 000 regional geological and mineral resources survey in Heilongjiang Province, the author carries out the zircon U-Pb isotopic dating for the granitic rocks in the area. The results show that the Triassic granite was formed in 224-229 Ma; while the Jurassic intrusive rock is dated as 202-193 Ma.

       

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