阿尔泰北部喀纳斯群碎屑岩锆石UPb同位素年龄及其意义

王星, 蔺新望, 赵端昌, 张亚峰, 菅坤坤, 杜彪, 朱伟鹏. 阿尔泰北部喀纳斯群碎屑岩锆石UPb同位素年龄及其意义[J]. 西北地质, 2016, 49(3): 13-27.
引用本文: 王星, 蔺新望, 赵端昌, 张亚峰, 菅坤坤, 杜彪, 朱伟鹏. 阿尔泰北部喀纳斯群碎屑岩锆石UPb同位素年龄及其意义[J]. 西北地质, 2016, 49(3): 13-27.
WANG Xing, LIN Xinwang, ZHAO Duanchang, ZHANG Yafeng, JIAN Kunkun, DU Biao, ZHU Weipeng. U-Pb Dating of Detrital Zircons from the Kanas Group in Northern Altay and Its Geological Significance[J]. Northwestern Geology, 2016, 49(3): 13-27.
Citation: WANG Xing, LIN Xinwang, ZHAO Duanchang, ZHANG Yafeng, JIAN Kunkun, DU Biao, ZHU Weipeng. U-Pb Dating of Detrital Zircons from the Kanas Group in Northern Altay and Its Geological Significance[J]. Northwestern Geology, 2016, 49(3): 13-27.

阿尔泰北部喀纳斯群碎屑岩锆石UPb同位素年龄及其意义

  • 基金项目: 中国地质调查局“阿尔泰成矿带喀纳斯和东准地区地质矿产调查”(121201011000150003)

U-Pb Dating of Detrital Zircons from the Kanas Group in Northern Altay and Its Geological Significance

  • 阿尔泰北部大面积出露的喀纳斯群为一套巨厚的浅变质陆缘碎屑岩,本次工作系统采集了锆石同位素年龄样品及岩石地球化学样品,其地球化学分析结果显示沉积物来源于被动大陆边缘环境;获得的碎屑锆石U-Pb同位素年龄资料中,最年轻的岩浆锆石年龄为(545.8±3.7)Ma,据此可将喀纳斯群的底界定为震旦系;较老的元古代锆石年龄(858±13 Ma及1 800~1 983Ma)暗示了物源区很可能存在前寒武纪大陆地壳基底。
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收稿日期:  2016-03-02
修回日期:  2016-05-23
刊出日期:  2016-09-15

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