冯丽霞, 张志诚, 韩宝福, 任荣, 李建锋, 苏犁. 2013: 内蒙古达茂旗花岗岩类LA-ICP-MS锆石U-Pb年龄及其地质意义. 地质通报, 32(11): 1737-1748.
    引用本文: 冯丽霞, 张志诚, 韩宝福, 任荣, 李建锋, 苏犁. 2013: 内蒙古达茂旗花岗岩类LA-ICP-MS锆石U-Pb年龄及其地质意义. 地质通报, 32(11): 1737-1748.
    FENG Li-xia, ZHANG Zhi-cheng, HAN Bao-fu, REN Rong, LI Jian-feng, SU Li. 2013: LA-ICP-MS zircon U-Pb ages of granitoids in Darhan Muminggan Joint Banner, Inner Mongolia, and their geological significance. Geological Bulletin of China, 32(11): 1737-1748.
    Citation: FENG Li-xia, ZHANG Zhi-cheng, HAN Bao-fu, REN Rong, LI Jian-feng, SU Li. 2013: LA-ICP-MS zircon U-Pb ages of granitoids in Darhan Muminggan Joint Banner, Inner Mongolia, and their geological significance. Geological Bulletin of China, 32(11): 1737-1748.

    内蒙古达茂旗花岗岩类LA-ICP-MS锆石U-Pb年龄及其地质意义

    LA-ICP-MS zircon U-Pb ages of granitoids in Darhan Muminggan Joint Banner, Inner Mongolia, and their geological significance

    • 摘要: 对内蒙古达茂旗北部构造单元的巴特敖包岛弧带2个花岗闪长岩岩体样品和南部构造单元一个花岗岩岩体的2件样品进行了LA-ICP-MS锆石U-Pb定年。北部构造单元采自2个花岗闪长岩岩体的样品锆石206Pb/238U年龄分别为468Ma±2Ma和452Ma±3Ma,代表了这2个岩体的侵位时间,表明古亚洲洋向华北克拉通之下俯冲不晚于468Ma±2Ma;南部构造单元采自同一花岗岩岩体的2件样品获得的锆石206Pb/238U年龄分别为268Ma±2Ma和264Ma±2Ma,和该单元西部岩体已有的锆石年龄相符。这为华北克拉通北缘岩浆作用研究提供了新的年代学证据。

       

      Abstract: This paper reports four zircon U-Pb ages of granitoids in Darhan Muminggan Joint Banner, Inner Mongolia. Two granodiorite samples from Bater magmatic arc in the northern part and two granite samples from a single pluton in the southern part were dated by LA-ICP-MS zircon U-Pb method so as to define their emplacement ages and provide constraints on the subduction and collisional events of the Paleo-Asian Ocean in the central part of Inner Mongolia. The two granodiorite samples yielded zircon U-Pb ages of 468Ma±2Ma and 452Ma±3Ma, respectively, indicating that the southward subduction of the paleo-Asian ocean beneath the North China Craton started at least at 468Ma, which resulted in the formation of Bater Obo magmatic arc, and the two granite samples gave zircon U-Pb ages of 268Ma±2Ma and 264Ma±2Ma, respectively, which are within the range of pre-existing age data from the western pluton, although the tectonic setting of the Middle Permian plutonism in the southern part is still uncertain.

       

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