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中国东部大陆边缘晚新生代构造演化及板块相互作用过程重建

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尚鲁宁, 张勇, 姚永坚, 吴浩, 胡刚, 田陟贤. 2020. 中国东部大陆边缘晚新生代构造演化及板块相互作用过程重建[J]. 中国地质, 47(5): 1323-1336. doi: 10.12029/gc20200503
引用本文: 尚鲁宁, 张勇, 姚永坚, 吴浩, 胡刚, 田陟贤. 2020. 中国东部大陆边缘晚新生代构造演化及板块相互作用过程重建[J]. 中国地质, 47(5): 1323-1336. doi: 10.12029/gc20200503
shu
SHANG Luning, ZHANG Yong, YAO Yongjian, WU Hao, HU Gang, TIAN Zhixian. 2020. Late Cenozoic evolution of East China continental margin and restoration of plate interaction processes[J]. Geology in China, 47(5): 1323-1336. doi: 10.12029/gc20200503
Citation: SHANG Luning, ZHANG Yong, YAO Yongjian, WU Hao, HU Gang, TIAN Zhixian. 2020. Late Cenozoic evolution of East China continental margin and restoration of plate interaction processes[J]. Geology in China, 47(5): 1323-1336. doi: 10.12029/gc20200503
shu

中国东部大陆边缘晚新生代构造演化及板块相互作用过程重建

  • 1.

    青岛海洋地质研究所, 山东 青岛 266071

  • 2.

    广州海洋地质调查局, 广东 广州 510075

  • 基金项目:
    中国地质调查局地质调查项目(DD20160137，DD20160138，DD20190236)与国家自然科学基金项目（41606050，91858208）共同资助
详细信息
    作者简介: 尚鲁宁, 男, 1986年生, 副研究员, 主要从事海域构造地质学研究; E-mail:shang1924@163.com
    通讯作者: 张勇, 男, 1970年生, 教授级高级工程师, 主要从事海洋基础地质调查与研究; E-mail:qimgzy@163.com

  • 中图分类号: P736.1

Late Cenozoic evolution of East China continental margin and restoration of plate interaction processes

  • 1.

    Qingdao Institute of Marine Geology, Qingdao 266071, Shandong, China

  • 2.

    Guangzhou Marine Geological Survey, Guangzhou 510075, Guangdong, China

  • Fund Project: Supported by Geological Survey Project (No. DD20160137, No. DD20160138, No. DD20190236) and National Natural Science Foundation of China (No. 41606050).
More Information
    Author Bio: SHANG Luning, male, born in 1986, associate researcher, mainly engages in the study of marine tectonics; E-mail:shang1924@163.com .
    Corresponding author: ZHANG Yong, male, born in 1970, senior researcher, mainly engages in marine regional geological survey and research; E-mail:qimgzy@163.com

    摘要

  • 晚新生代中国东部大陆边缘的构造活动主要集中于东海东缘。中新世以来菲律宾海板块俯冲、冲绳海槽弧后张裂、台湾弧-陆碰撞等一系列重大构造过程，塑造了现今琉球沟-弧-盆体系、台湾碰撞造山带和南海东北部的构造-地貌格局。本文基于对重磁和多道地震资料的解译，并结合前人研究成果，恢复了冲绳海槽构造演化史，阐明了冲绳海槽弧后张裂和台湾弧-陆碰撞之间的关系。在此基础上，重建了中新世以来欧亚板块、菲律宾海板块、南海板块之间的相互作用过程模型。本研究有助于进一步理解板块汇聚背景下东亚大陆边缘深部动力-热力过程对浅部构造格局变迁的制约和影响。

    The tectonic activities of the continental margin of eastern China during the Late Cenozoic were mainly concentrated on the eastern margin of the East China Sea. Since the Miocene, a series of major tectonic processes, such as the subduction of the Philippine plate, the back-arc rifting of the Okinawa Trough and the Taiwan arc-continent collision, have shaped the present tectonic-geomorphological patterns of the Ryukyu trench-arc-back-arc basin system, the Taiwan collision orogenic belt and the northeastern South China Sea. Based on the interpretation of gravity, magnetism and multi-channel seismic data and combined with previous research results, the authors restored the tectonic evolution history of the Okinawa Trough and clarified the relationship between the back-arc tension of the Okinawa Trough and the Taiwan arc-land collision. On such a basis, the interaction processes between the Eurasian plate, the Philippine Sea plate and the South China Sea plate since Miocene were reconstructed, and a new model of plate interaction was proposed. This work is helpful to the further understanding of the constraints and effects of deep dynamic and thermal processes on shallow tectonic framework changes in the context of plate convergence on the East Asian continental margin.

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  • 图 1  冲绳海槽及邻区构造纲要图(据Kimura, 1985; Sibuet et al., 1987, 1998; Hsu et al., 2001; 赵金海, 2004; Huang et al., 2008修改; 水深数据来源www.marine-geo.org)

    Figure 1. 

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    图 2  冲绳海槽海底地www.marine-geo.org形及地震剖面、钻井位置图(红色实线为地震剖面，水深数据来源www.marine-geo.org)

    Figure 2. 

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    图 3  冲绳海槽及邻区空间重力异常图(a)和ΔT 磁异常图(b)

    Figure 3. 

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    图 4  冲绳海槽及邻区地震地层划分和对比

    Figure 4. 

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    图 5  冲绳海槽中段宽缓陆坡区地层结构（红线为断裂，剖面位置见图 2）

    Figure 5. 

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    图 6  冲绳海槽中段Ho盆地构造特征（红线为断裂，剖面位置见图 2）

    Figure 6. 

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    图 7  冲绳海槽中段陡峭陆坡区的地层结构（红线为断裂，剖面位置见图 2）

    Figure 7. 

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    图 8  地震剖面揭示的钓鱼岛隆起带中段基底构造特征（红线为断裂，剖面位置见图 2）

    Figure 8. 

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    图 9  冲绳海槽南段基底构造特征和沉积层结构（红线为断裂，剖面位置见图 2）

    Figure 9. 

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    图 10  地震剖面揭示的冲绳海槽南段西侧陆架边缘结构特征（红线为断裂，剖面位置见图 2）

    Figure 10. 

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    图 11  晚新生代冲绳海槽及吕宋—台湾碰撞带的形成演化

    Figure 11. 

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收稿日期:  2020-04-03
修回日期:  2020-08-05
刊出日期:  2020-10-25

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