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    广西运动在华南板块北缘的构造响应:来自生物地层学方面的证据

    王欣 高晓峰 查显锋

    王欣, 高晓峰, 查显锋, 2024. 广西运动在华南板块北缘的构造响应:来自生物地层学方面的证据. 地球科学, 49(9): 3199-3211. doi: 10.3799/dqkx.2023.115
    引用本文: 王欣, 高晓峰, 查显锋, 2024. 广西运动在华南板块北缘的构造响应:来自生物地层学方面的证据. 地球科学, 49(9): 3199-3211. doi: 10.3799/dqkx.2023.115
    Wang Xin, Gao Xiaofeng, Zha Xianfeng, 2024. Tectonic Response of the Kwangsian Orogeny in the Northern Margin of the South China Block: Evidences from Biostratigraphy. Earth Science, 49(9): 3199-3211. doi: 10.3799/dqkx.2023.115
    Citation: Wang Xin, Gao Xiaofeng, Zha Xianfeng, 2024. Tectonic Response of the Kwangsian Orogeny in the Northern Margin of the South China Block: Evidences from Biostratigraphy. Earth Science, 49(9): 3199-3211. doi: 10.3799/dqkx.2023.115

    广西运动在华南板块北缘的构造响应:来自生物地层学方面的证据

    doi: 10.3799/dqkx.2023.115
    基金项目: 

    中国地质调查局项目 DD20243411

    中国地质调查局项目 DD20240029

    中国地质调查局项目 DD20230553

    中国地质调查局项目 DD20230005

    中国地质调查局项目 DD20230215

    中国科学院南京地质古生物研究所现代古生物学和地层学国家重点实验室开放课题基金项目 213121

    陕西省自然科学基础研究计划面上项目 2022JM⁃149

    陕西省自然科学基础研究计划面上项目 2023⁃JC⁃ZD⁃15

    陕西省自然科学基础研究计划面上项目 2022JC⁃DW5⁃01

    陕西省自然科学基础研究计划面上项目 2023⁃JC⁃YB⁃268

    国家自然科学基金项目 42242201

    国家自然科学基金项目 40872004

    国家自然科学基金项目 41302006

    详细信息
      作者简介:

      王欣(1984-),男,博士,副研究员,主要从事古生物学与地层学相关研究.ORCID:0000-0002-9495-8636. E-mail:wx200315046@163.com

      通讯作者:

      查显锋,E-mail:zha_xianfeng@126.com

    • 中图分类号: P52

    Tectonic Response of the Kwangsian Orogeny in the Northern Margin of the South China Block: Evidences from Biostratigraphy

    • 摘要: 广西运动的构造作用范围是否涵盖华南板块北缘尚存在不同认识,并成为了制约相关构造动力学机制研究的瓶颈.此次研究聚焦北大巴山地区,以精确的笔石生物地层序列为标尺,同时综合岩石学特征认为,广西运动在华南板块北缘存在构造‒沉积响应,其构造启动时间为志留系特列奇阶Spirograptus turriculatus笔石带所代表的时限(~435 Ma),与“扬子上升”第一幕的时限基本一致.在华南板块北缘,广西运动在特列奇阶Oktavites spiralis-Cyrtograptus lapworthi笔石带所涵盖的时间范围内第一次到达构造活动峰值(~433 Ma),期间还伴随着大规模的岩浆活动.本研究进一步扩大了广西运动的构造作用范围,同时也为相关的构造发生模式和动力学机制研究提供了更多的思路和参考,即华南与华北碰撞的远程效应可能是广西运动重要的构造驱动力之一.

       

    • 图  1  研究区域地质简图及剖面位置

      Fig.  1.  Geological map showing the locations for sections in this study

      图  2  研究区域剖面综合柱状图

      Fig.  2.  Biostratigraphy and lithological characters of the studied sections in the Ziyang⁃Langao area

      图  3  紫阳‒岚皋地区志留纪笔石类群

      a. Coronograptus cyphus(Lapworth,1876),斑鸠关剖面,斑鸠关组,Gr26163;b. Demirastrites triangulatus(Harkness,1851),斑鸠关剖面,斑鸠关组,Gr26841;c. Lituigraptus convolutus(Hisinger,1837),紫黄剖面,龙马溪组,Gr25143;d.(1)Stimulograptus halli(Barrande,1850),(2)Demirastrites raitzhainiensis(Eisel,1899),(3)Spirograptus turriculatus(Barrande,1850),(4)Spirograptus guerichiLoydell,Storch and Melchin,1993),紫黄剖面,崔家沟组,Gr24857;e. Oktavites planus(Barrande,1850),紫黄剖面,崔家沟组,Gr24970;f. Spirograptus guerichi,紫黄剖面,龙马溪组,Gr22608;g. Oktavites contortus(Perner,1897),紫黄剖面,龙马溪组,Gr23227;比例尺代表 1 mm

      Fig.  3.  Silurian graptolite species from the Ziyang⁃Langao area

      图  4  紫阳‒岚皋地区志留纪笔石类群

      a.Spirograptus turriculatus(Barrande,1850),芭蕉口剖面,陡山沟组,Gr20293;b.Streptograptus exiguus(Lapworth,1876),芭蕉口剖面,陡山沟组,Gr21416;c.Monograptus crispus(Lapworth,1876),芭蕉口剖面,陡山沟组,Gr25891;d.Cyrtograptus lapworthi(Tullberg,1883),芭蕉口剖面,伍峡河组,Gr20166;e.Oktavites spiralis(Geinitz,1842),龙潭剖面,陡山沟组,Gr21424;f.Cyrtograptus sakmaricus(Koren,1968),桥西剖面,伍峡河组,Gr20143;比例尺代表 1 mm;图 3和图 4化石标本均保存在中国地质调查局西安地质调查中心

      Fig.  4.  Silurian graptolite species from the Ziyang–Langao area

      图  5  广西运动构造动力学发生模式

      修改自徐亚军和杜远生(2018)王怿等(2021)

      Fig.  5.  Tectonic dynamics model of the Kwangsian Orogeny

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    出版历程
    • 收稿日期:  2023-03-23
    • 网络出版日期:  2024-10-16
    • 刊出日期:  2024-09-25

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