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    扬子克拉通北缘中元古代神农架群构造属性:来自碎屑锆石U-Pb年代学的约束

    卢山松 童喜润 吴年文 江拓 王志先 周涛 王江 邱啸飞

    卢山松, 童喜润, 吴年文, 江拓, 王志先, 周涛, 王江, 邱啸飞, 2025. 扬子克拉通北缘中元古代神农架群构造属性:来自碎屑锆石U-Pb年代学的约束. 地球科学, 50(7): 2613-2627. doi: 10.3799/dqkx.2025.088
    引用本文: 卢山松, 童喜润, 吴年文, 江拓, 王志先, 周涛, 王江, 邱啸飞, 2025. 扬子克拉通北缘中元古代神农架群构造属性:来自碎屑锆石U-Pb年代学的约束. 地球科学, 50(7): 2613-2627. doi: 10.3799/dqkx.2025.088
    Lu Shansong, Tong Xirun, Wu Nianwen, Jiang Tuo, Wang Zhixian, Zhou Tao, Wang Jiang, Qiu Xiaofei, 2025. Mesoproterozoic Tectonic Characteristics of Shennongjia Group in Northern Margin of Yangtze Craton: Constraints from Detrital Zircon U-Pb Geochronology. Earth Science, 50(7): 2613-2627. doi: 10.3799/dqkx.2025.088
    Citation: Lu Shansong, Tong Xirun, Wu Nianwen, Jiang Tuo, Wang Zhixian, Zhou Tao, Wang Jiang, Qiu Xiaofei, 2025. Mesoproterozoic Tectonic Characteristics of Shennongjia Group in Northern Margin of Yangtze Craton: Constraints from Detrital Zircon U-Pb Geochronology. Earth Science, 50(7): 2613-2627. doi: 10.3799/dqkx.2025.088

    扬子克拉通北缘中元古代神农架群构造属性:来自碎屑锆石U-Pb年代学的约束

    doi: 10.3799/dqkx.2025.088
    基金项目: 

    国家自然科学基金项目 42272229

    国家自然科学基金项目 U2344210

    国家自然科学基金项目 41303026

    古生物与地质环境演化湖北省重点实验室开放研究基金项目 PEL-202205

    详细信息
      作者简介:

      卢山松(1986—), 男, 高级工程师, 硕士, 主要从事同位素分析测试和地球化学示踪研究. ORCID: 0009-0005-3236-3783. E-mail: lushansong@mail.cgs.gov.cn

    • 中图分类号: P597

    Mesoproterozoic Tectonic Characteristics of Shennongjia Group in Northern Margin of Yangtze Craton: Constraints from Detrital Zircon U-Pb Geochronology

    • 摘要:

      为了解扬子克拉通北缘中元古代地质构造演化过程,对扬子克拉通北缘神农架群矿石山组、石槽河组、台子组沉积地层进行了碎屑锆石U-Pb年龄分析.结果显示,神农架群碎屑锆石的峰值年龄在~1.60 Ga、2.00~2.10 Ga和2.50~ 2.70 Ga,同时还存在少量2.20~2.30 Ga和 > 2.80 Ga锆石年龄.碎屑锆石年龄谱的结果显示神农架群的沉积时限应为1.10~1.60 Ga.通过对比扬子克拉通中元古代地层和扬子陆核区碎屑锆石年龄谱,扬子克拉通西缘和北缘总体不具有相似的年龄分布特征,指示二者在中元古代可能具有相对独立的构造演化过程;神农架群和打鼓石群具有相似的年龄分布,但二者在1.40~1.60 Ga期间不同的锆石年龄峰值指示二者在中元古代可能经历了不同的演化过程.结合前人的研究资料,扬子克拉通在中元古代之前可能呈现为多个相互独立的陆块,并在古元古代‒中元古代的构造演化过程中先后拼合到扬子克拉通基底中.

       

    • 图  1  神农架地区地质简图(据Qiu et al., 2011修改)

      Fig.  1.  Simplified geological map of Shennongjia region (modified from Qiu et al., 2011)

      图  2  神农架地区中元古代地层柱状图及采样点位

      李怀坤等(2013a)修改.1. 砾岩;2. 砂砾岩;3. 砂岩;4. 粉砂岩;5. 页岩/板岩;6. 燧石;7. 石灰岩;8. 白云岩;9. 角砾状白云岩;10. 硅质条带白云岩;11. 叠层石白云岩;12. 火山岩;13. 凝灰岩;14. 整合接触关系;15. 平行不整合接触关系;16. 采样点位

      Fig.  2.  Mesoproterozoic stratigraphic histogram of the Shennongjia area and the sampling locations

      图  3  神农架群部分锆石阴极发光(CL)照片

      Fig.  3.  Cathodoluminescence (CL) photographs of part zircons from the Shennongjia Group

      图  4  矿石山组、石槽河组、台子组及神农架群碎屑锆石年龄谱

      Fig.  4.  Age spectra of detrital zircons from the Kuangshishan Formation, Shicaohe Formation, Taizi Formation, and Shennongjia Group

      图  5  扬子克拉通中元古代地层和扬子陆核区碎屑锆石年龄谱

      昆阳群数据引自李怀坤等(2013b)纪星星等(2016)Sun et al.(2021)刘星宇(2021),会理群数据引自季雷(2015)Cui et al.(2021)Sun et al.(2022),东川群数据引自Zhao et al.(2010)李怀坤等(2013b)Wang and Zhou(2014)季雷(2015)Liu et al.(2018)任光明等(2020)肖剑等(2021),打鼓石群数据引自孔令耀等(2017)刘浩等(2017)Huang et al.(2021),扬子陆核区数据引自Zhang et al.(2006)Liu et al.(2008a)Hofmann et al.(2011)Wang et al.(2013b),神农架群引自肖志斌(2012)李怀坤等(2013a)徐大良等(2016)

      Fig.  5.  Age spectra of detrital zircons from the Mesoproterozoic stratigraphy of the Yangtze Craton and the Yangtze continental nucleus

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    • 收稿日期:  2025-03-10
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