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    郭华春, 钟莉, 李丽群. 2006: 哈尔里克山口门子地区石英闪长岩锆石SHRIMP U-Pb测年及其地质意义. 地质通报, 25(8): 928-931.
    引用本文: 郭华春, 钟莉, 李丽群. 2006: 哈尔里克山口门子地区石英闪长岩锆石SHRIMP U-Pb测年及其地质意义. 地质通报, 25(8): 928-931.
    shu
    2006: Zircon SHRIMP U-Pb dating of quartz diorite in the Koumenzi area, Karlik Mountains, East Tianshan, Xinjiang, China, and its geological significance. Geological Bulletin of China, 25(8): 928-931.
    Citation: 2006: Zircon SHRIMP U-Pb dating of quartz diorite in the Koumenzi area, Karlik Mountains, East Tianshan, Xinjiang, China, and its geological significance. Geological Bulletin of China, 25(8): 928-931.
    shu

    哈尔里克山口门子地区石英闪长岩锆石SHRIMP U-Pb测年及其地质意义

    Zircon SHRIMP U-Pb dating of quartz diorite in the Koumenzi area, Karlik Mountains, East Tianshan, Xinjiang, China, and its geological significance

      摘要
    • 摘要: 哈尔里克山口门子一带原划石炭纪石英闪长岩的锆石SHRIMPU-Pb年龄为429.6Ma±6.2Ma,其围岩原被置于下中泥盆统,根据1∶5万区域地质调查和前人的资料,将其重新厘定为奥陶系。结合区域上该构造单元近年内获得的新成果,提出准噶尔南缘地区加里东构造岩浆带已越过卡拉麦里-麦钦乌拉断裂、广泛发育于哈尔里克-大南湖华力西岛弧带上的认识。

       

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