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超大陆与全球板块重建派别

李三忠 ,  余珊 ,  赵淑娟 ,  张国伟 ,  刘鑫 ,  曹花花 ,  许立青 ,  戴黎明 ,  李涛

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文章导航 > 海洋地质与第四纪地质  > 2014 >  34(6): 97-117
李三忠, 余珊, 赵淑娟, 张国伟, 刘鑫, 曹花花, 许立青, 戴黎明, 李涛. 超大陆与全球板块重建派别[J]. 海洋地质与第四纪地质, 2014, 34(6): 97-117. doi: 10.3724/SP.J.1140.2014.06097
引用本文: 李三忠, 余珊, 赵淑娟, 张国伟, 刘鑫, 曹花花, 许立青, 戴黎明, 李涛. 超大陆与全球板块重建派别[J]. 海洋地质与第四纪地质, 2014, 34(6): 97-117. doi: 10.3724/SP.J.1140.2014.06097
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LI Sanzhong, YU Shan, ZHAO Shujuan, ZHANG Guowei, LIU Xin, CAO Huahua, XU Liqing, DAI Liming, LI Tao. SCHOOLS OF THOUGHT ON SUPERCONTINENT AND GLOBAL PLATE RECONSTRUCTION[J]. Marine Geology & Quaternary Geology, 2014, 34(6): 97-117. doi: 10.3724/SP.J.1140.2014.06097
Citation: LI Sanzhong, YU Shan, ZHAO Shujuan, ZHANG Guowei, LIU Xin, CAO Huahua, XU Liqing, DAI Liming, LI Tao. SCHOOLS OF THOUGHT ON SUPERCONTINENT AND GLOBAL PLATE RECONSTRUCTION[J]. Marine Geology & Quaternary Geology, 2014, 34(6): 97-117. doi: 10.3724/SP.J.1140.2014.06097
shu

超大陆与全球板块重建派别


doi: 10.3724/SP.J.1140.2014.06097
详细信息

  • 1. 中国海洋大学海洋地球科学学院, 青岛 266100;

  • 2. 海底科学与探测技术教育部重点实验室, 青岛 266100;

  • 3. 西北大学地质学系, 西安 710069

    • 作者简介:

    李三忠(1968-),男,博士,教授,博导,从事构造地质学及海洋地质学的教学和研究工作,E-mail:sanzhong@ouc.edu.cn

  • 基金项目:

    国家自然科学基金重大项目(41190072,41190070)；国家杰出青年基金项目(41325009)

  • 中图分类号: P731

SCHOOLS OF THOUGHT ON SUPERCONTINENT AND GLOBAL PLATE RECONSTRUCTION

More Information

  • 1. College of Marine Geosciences, Ocean University of China, Qingdao 266100, China;

  • 2 Key Lab of Submarine Geosciences and Prospecting Technique, Ministry of Education, Qingdao 266100, China;

  • 3. Department of Geology, Northwest University, Xi'an 710069, China

  • 摘要: 板块重建是全球构造研究的核心和前沿,而且该研究自Wegener开始就以多学科集成综合为特征,随着21世纪进入大数据时代,其多学科交叉协同创新特色更为鲜明。但当前板块重建各派依然发挥各自特长,在板块重建领域,显示出其某方面的积累和特色,总体可分成14大派别:(1)最早利用计算机从事板块重建的Scotese群体;(2)仅依据古地磁极移为依据进行重建的Piper群体;(3)以Golonka为首的群体侧重岩相古地理、古环境相结合的板块重建;(4)重点对东南亚和西太平洋地区中生代-新生代进行板块重建的Robert Hall群体;(5)发展了板块和地质重建程序的Lawrence Lawver群体;(6)以古生物地理和古气候为特色的陈旭群体;(7)以海底磁条带和古水深重建为特色的Müller群体;(8)以古地貌、动力地形和沉积岩相重建为特色的Blakey群体;(9)以古地磁条带和蛇绿岩对比为特色的Stampfli群体;(10)以古地磁极移和地质综合对比为特色的LI Zhengxiang群体;(11)以与深部地球物理(层析成像)相结合为特色的Torsvik群体;(12)以碎屑锆石年龄谱对比为特色的Cawood群体;(13)以变质动力学和碰撞造山带事件对比为特色的Zhao Guochun群体;(14)打破刚性板块理念,开启可变形板块和动力地形重建的Michael Gurnis群体。各家在重建板块的时代上也有所侧重,从20世纪初Wegener提出2.5亿年左右的Pangea重建开始,到20世纪90年代初10亿年左右的Rodinia超大陆重建,再到20世纪90年代末Zhao Guochun和Rogers古元古代18亿年的Columbia超大陆重建。
    Abstract: Plate reconstruction, as a multidisciplinary scientific integration, has become the core and frontier of global tectonics research since A. Wegener. In the big data era as the 21st century, the multidisciplinary collaborative innovation is even more distinctive. However, any expert has his own specialized fields as well as limitation, group endeavor is required for plate reconstruction. There are fourteen schools of thought in general:(1) The Scotese group being an earlier group based on computer techniques; (2) The Piper group solely based on paleomagnetic polar wandering for plate reconstruction; (3) The group led by Golonka focusing on the combination of lithofacies palaeogeography and paleoenvironmental reconstruction; (4) The Robert Hall group on plate reconstruction specifically in the western Pacific and the southeast Asia; (5) The Lawrence Lawver group with special interest in developing plate reconstruction software; (6) The Chen Xu group featured by palaeobiogeography and paleoclimate; (7) The Mueller group based on magnetic lineations and the rebuilding of ancient ocean bythemetry; (8) The Barsley group focusing on the ancient topography, terrain and sedimentary facies; (9) The Stampfli group to reconstruct the ancient paleomagnetic lineations based on ophiolites; (10) The Li Zhengxiang group based on paleomagnetic polar wandering and integrated correlation of geological events; (11) The Torsvik group focusing on deep-seated geophysical (tomography) data in corporation with paleomagentics; (12) The Cawood group making plate reconstruction based on detrital zircon age spectrums; (13) The Zhao Guochun group devoting to degenerated dynamics and collision orogenic events; (14) The Michael Gurnis group who broke the concept of rigid plate for dynamic topography reconstruction and deformed plate reconstruction. Each group also has its interest and emphasis on specific era. For examples, Since A. Wegener at the beginning of the last century up to now, many groups have been interesting in the reconstruction of the Pangea supercontinent 250 Ma; since early 1990s, more work has been rendered to the plate reconstruction of the Rodinia supercontient 1.0 Ga; and since the end of 1990s, Zhao Guochun and Rogers have paid more attention to the reconstruction of the Columbia supercontinent in Paleoproterozoic 1.8 Ga.
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出版历程
  • 收稿日期:  2013-12-30
  • 修回日期:  2014-05-20

超大陆与全球板块重建派别

doi: 10.3724/SP.J.1140.2014.06097
  • 1. 中国海洋大学海洋地球科学学院, 青岛 266100;
  • 2. 海底科学与探测技术教育部重点实验室, 青岛 266100;
  • 3. 西北大学地质学系, 西安 710069
    • 作者简介:

    李三忠(1968-),男,博士,教授,博导,从事构造地质学及海洋地质学的教学和研究工作,E-mail:sanzhong@ouc.edu.cn

  • 收稿日期: 2013-12-30
  • 修回日期: 2014-05-20
基金项目:

国家自然科学基金重大项目(41190072,41190070)；国家杰出青年基金项目(41325009)

  • 中图分类号: P731

摘要: 板块重建是全球构造研究的核心和前沿,而且该研究自Wegener开始就以多学科集成综合为特征,随着21世纪进入大数据时代,其多学科交叉协同创新特色更为鲜明。但当前板块重建各派依然发挥各自特长,在板块重建领域,显示出其某方面的积累和特色,总体可分成14大派别:(1)最早利用计算机从事板块重建的Scotese群体;(2)仅依据古地磁极移为依据进行重建的Piper群体;(3)以Golonka为首的群体侧重岩相古地理、古环境相结合的板块重建;(4)重点对东南亚和西太平洋地区中生代-新生代进行板块重建的Robert Hall群体;(5)发展了板块和地质重建程序的Lawrence Lawver群体;(6)以古生物地理和古气候为特色的陈旭群体;(7)以海底磁条带和古水深重建为特色的Müller群体;(8)以古地貌、动力地形和沉积岩相重建为特色的Blakey群体;(9)以古地磁条带和蛇绿岩对比为特色的Stampfli群体;(10)以古地磁极移和地质综合对比为特色的LI Zhengxiang群体;(11)以与深部地球物理(层析成像)相结合为特色的Torsvik群体;(12)以碎屑锆石年龄谱对比为特色的Cawood群体;(13)以变质动力学和碰撞造山带事件对比为特色的Zhao Guochun群体;(14)打破刚性板块理念,开启可变形板块和动力地形重建的Michael Gurnis群体。各家在重建板块的时代上也有所侧重,从20世纪初Wegener提出2.5亿年左右的Pangea重建开始,到20世纪90年代初10亿年左右的Rodinia超大陆重建,再到20世纪90年代末Zhao Guochun和Rogers古元古代18亿年的Columbia超大陆重建。

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