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赣南南华纪变质沉凝灰岩的碎屑锆石U-Pb年代学及其对裂谷盆地形成时间的限定

赵芝, 臧雯蕊, 王臻, 陈振宇, 陈斌锋, 邹新勇. 2021. 赣南南华纪变质沉凝灰岩的碎屑锆石U-Pb年代学及其对裂谷盆地形成时间的限定[J]. 中国地质, 48(2): 564-579. doi: 10.12029/gc20210215
引用本文: 赵芝, 臧雯蕊, 王臻, 陈振宇, 陈斌锋, 邹新勇. 2021. 赣南南华纪变质沉凝灰岩的碎屑锆石U-Pb年代学及其对裂谷盆地形成时间的限定[J]. 中国地质, 48(2): 564-579. doi: 10.12029/gc20210215
ZHAO Zhi, ZANG Wenrui, WANG Zhen, CHEN Zhenyu, CHEN Bingfeng, ZOU Xinyong. 2021. Detrital zircon U-Pb dating of Nanhua meta-tuffite in South Jiangxi and constraint on the time limit of the rift basin[J]. Geology in China, 48(2): 564-579. doi: 10.12029/gc20210215
Citation: ZHAO Zhi, ZANG Wenrui, WANG Zhen, CHEN Zhenyu, CHEN Bingfeng, ZOU Xinyong. 2021. Detrital zircon U-Pb dating of Nanhua meta-tuffite in South Jiangxi and constraint on the time limit of the rift basin[J]. Geology in China, 48(2): 564-579. doi: 10.12029/gc20210215

赣南南华纪变质沉凝灰岩的碎屑锆石U-Pb年代学及其对裂谷盆地形成时间的限定

  • 基金项目:
    中央级公益性科研院所基本科研业务费专项基金(K1506和YYWF201527)资助
详细信息
    作者简介: 赵芝, 女, 1984年生, 高级工程师, 主要从事稀土矿床成矿理论研究; E-mail: zhaozhi_sun@163.com.
    通讯作者: 陈振宇, 男, 1978年生, 教授级高级工程师, 主要从事矿物学和微束分析; E-mail: czy7803@126.com
  • 中图分类号: P578.496;P597.3

Detrital zircon U-Pb dating of Nanhua meta-tuffite in South Jiangxi and constraint on the time limit of the rift basin

  • Fund Project: Supported by Central Level, Scientific Research Institutes for Basic R & D Special Fund Business (No.K1506 and No.YYWF201527)
More Information
    Author Bio: ZHAO Zhi, female, born in 1984, senior engineer, engaged in the mineralization of rare earth deposits in China; E-mail: zhaozhi_sun@163.com. .
    Corresponding author: CHEN Zhengyu, male, born in 1978, senior engineer, engaged in the mineralogy and microbeam analysis, E-mail: czy7803@126.com
  • 江西省宁都某地新元古代浅变质岩风化壳中赋存离子吸附型稀土矿,文章对某矿区内原定青白口纪库里组的2件变质沉凝灰岩样品进行了碎屑锆石LA-ICP-MS U-Pb年代学研究,获得了88组和110组谐和年龄。2件样品的碎屑锆石年龄区间相似,主要分布在:810~780 Ma,峰值年龄为798 Ma(n=55);748~727 Ma,峰值年龄为737 Ma(n=127);691~667 Ma,峰值年龄为680 Ma(n=6),此外还有少量的年龄分布在2.85~1.08 Ga。认为,变质沉凝灰岩样品的沉积时代可能为南华纪,地层应归属为上施组;物源可能来自江南造山带东段(赣东北—皖南—浙西)青白口纪晚期—南华纪的火山-沉积岩;赣南区域上同时期的巨厚海相火山-碎屑沉积可能形成于华南古大陆裂解之后的裂谷盆地,赣南次级裂谷盆地的沉积时限为810~727 Ma。

  • 加载中
  • 图 1  江西省中—新元古代地层分布略图(据刘亚光,1997修改)

    Figure 1. 

    图 2  江西省宁都地区地质图(据福建省冶金工业局,1972和南方工业学校,1997修编)

    Figure 2. 

    图 3  用于碎屑锆石U-Pb测年的变质沉凝灰岩样品的采集层位示意图(据南方工业学校,1997绘编)

    Figure 3. 

    图 4  江西省宁都地区变质沉凝灰岩的野外及显微镜下特征

    Figure 4. 

    图 5  江西省宁都地区变质沉凝灰岩中碎屑锆石阴极发光图像及年龄

    Figure 5. 

    图 6  江西省宁都地区变质沉凝灰岩中的碎屑锆石U-Pb年龄谐和图(a, c)及相对频率图(b, d)

    Figure 6. 

    图 7  江西及其周边青白口纪—南华纪地层对比

    Figure 7. 

    表 1  江西省宁都变质沉凝灰岩的LA-ICPMS碎屑锆石U-Pb年龄测试结果

    Table 1.  LA-ICPMS detrital zircon U-Pb dating results of the meta-tuffites in Ningdu County of Jiangxi Province

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出版历程
收稿日期:  2018-09-10
修回日期:  2019-03-20
刊出日期:  2021-04-25

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