新生代大陆板内伸展盆—山耦合与大陆碰撞效应——以渤海湾盆地济阳坳陷、周缘隆起及边界断裂构造演化为例

李理, 赵利, 钟大赉. 新生代大陆板内伸展盆—山耦合与大陆碰撞效应——以渤海湾盆地济阳坳陷、周缘隆起及边界断裂构造演化为例[J]. 地质科学, 2013, 48(2): 406-418. doi: 10.3969/j.issn.0563-5020.2013.02.006
引用本文: 李理, 赵利, 钟大赉. 新生代大陆板内伸展盆—山耦合与大陆碰撞效应——以渤海湾盆地济阳坳陷、周缘隆起及边界断裂构造演化为例[J]. 地质科学, 2013, 48(2): 406-418. doi: 10.3969/j.issn.0563-5020.2013.02.006
Li Li, Zhao Li, Zhong Dalai. Cenozoic continental intraplate extension basin-mountain coupling and continental collision: Evidences from Bohai Bay Basin,its peripheral mountain and Tancheng-Lujiang fault[J]. Chinese Journal of Geology, 2013, 48(2): 406-418. doi: 10.3969/j.issn.0563-5020.2013.02.006
Citation: Li Li, Zhao Li, Zhong Dalai. Cenozoic continental intraplate extension basin-mountain coupling and continental collision: Evidences from Bohai Bay Basin,its peripheral mountain and Tancheng-Lujiang fault[J]. Chinese Journal of Geology, 2013, 48(2): 406-418. doi: 10.3969/j.issn.0563-5020.2013.02.006

新生代大陆板内伸展盆—山耦合与大陆碰撞效应——以渤海湾盆地济阳坳陷、周缘隆起及边界断裂构造演化为例

详细信息
    作者简介:

    李理,女,1967年1月生,博士,教授,构造地质学专业。E-mail:lilywmwys@upc.edu.cn

  • 中图分类号: P542

Cenozoic continental intraplate extension basin-mountain coupling and continental collision: Evidences from Bohai Bay Basin,its peripheral mountain and Tancheng-Lujiang fault

  • 新生代印欧大陆碰撞引发了中国西部前缘大规模多阶段地壳挤压缩短、构造变形与隆升及岩浆事件,在中国东部,新生代山脉的抬升、盆地的伸展、沉降,以及郯庐断裂带新生代的活动与青藏高原的隆升具有准同时性,伸展盆地—伸展山脉之间存在耦合关系。这种对应关系呈"幕式"变化,主要表现在印欧大陆碰撞岩石圈增厚、构造变形和抬升的高峰时期,对应盆地岩石圈伸展、减薄、快速构造沉降以及郯庐断裂带活动等阶段,当构造转入相对稳定(松弛)时期,表现为高原剥蚀夷平、岩浆活动频繁以及盆地构造沉降速率减缓等阶段。从全球板块构造的角度来看,中国西部、东部新生代挤压、伸展和走滑活动属同一动力学体系条件下的耦合关系,驱动力可能是两大板块碰撞、深部地幔脉动上涌以及新生代太平洋板块与欧亚板块俯冲和速率变化的共同作用。
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收稿日期:  2012-12-20
修回日期:  2013-01-25
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