地球科学进展 ›› 2000, Vol. 15 ›› Issue (2): 147 -153. doi: 10.11867/j.issn.1001-8166.2000.02.0147

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大别—郯庐—苏鲁造山带复合旋转拼贴作用
肖文交 ,周火兆秀 ,杨振宇 ,赵西西   
  1. ①中国科学院地质研究所岩石圈构造演化开放研究实验室,北京 100029;②地质矿产部航测遥感中心,北京 100083;③中国地质科学院地质力学研究所,北京 100081;④加州大学Santa Cruz分校,美国加州 CA95064
  • 收稿日期:1999-02-12 修回日期:1999-05-03 出版日期:2000-04-01
  • 通讯作者: 肖文交,男,1967年12月生,副研究员,主要从事碰撞造山带大地构造学研究。
  • 基金资助:

    国家自然科学基金项目“大别—苏鲁地区构造格局的古地磁与构造地质学研究”(编号:49672148)、“中国显生宙古地磁极移曲线的建立
    与地块运动的研究(编号:49334050)、中国科学院“百人计划”及中国博士后科学基金资助。

MULTIPLE ROTATION AND AMALGAMATION PROCESSES OF DABIE-TANLU-SULU OROGEN

XIAO Wenjiao ,ZHOU Yaoxiu ,YANG Zhenyu ,ZHAO Xixi   

  1. ①Lab of Lithos Tect Evol,Institute of Geology,Chinese Academy of Sciences,Beijing100029,China;②Aeromagnetic&Remote Sensing Center,Ministry of Land&Resources,Beijing100083,China;③Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing100081,China;④Santa Cruz School,University of California,CA95064,USA
  • Received:1999-02-12 Revised:1999-05-03 Online:2000-04-01 Published:2000-04-01

郯庐断裂带的成生演化与含超高压变质带(UHP)的大别及苏鲁造山带存在较密切的时空关系。郯庐断裂带所在的构造位置应是晚二叠世华北与扬子地块碰撞时的根带。UHP岩石的折返过程可能发生于华北、扬子地块的大角度旋转、拼合过程中。在华北与扬子地块的造山后期或者造山期后的构造变形中所记录的构造形迹经晚中生代以来的中国东部构造变形叠加而逐渐呈现复杂的构造组合,所谓“郯庐断裂带”的走滑平移即其中的一种运动方式。华北与扬子地块碰撞造山作用与陆内变形最终造就了大别—郯庐—苏鲁复合造山带。

 The formation and evolution of the Tancheng-Lujiang fault has close spatial-temporal relationship with the Dabie-Sulu UHP-bearing orogen.The tectonic setting of the Tancheng-Lujiang fault is located at the root zone of the collision between north and south China blocks which took place in the Early Permian time.The collision is characterized by the process of large-scale rotation and amalgamation,in which exhumation of the UHP rocks might happen.The deformational record of the late orogeny and/or post-orogeny which was reworked by late Mesozoic deformation in south China presents complicated structural assemblage, among which the strike-slip faulting of the Tancheng-Lujiang fault is considerable.The collisional orogenesis between north and south China blocks and intra-continental deformation finally
led to the formation of the multiple Dabie-Tanlu-Sulu orogen.

中图分类号: 

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