ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
论华南(北部)前震旦纪基本构造格局与演化
  
关键词:northern South China  Pre-Sinian  tectonic framework
基金项目:国家地质调查项目:H50E016012(田坂街幅)、H50E017012(游城幅),1∶5万区域地质调查(20001300002051)
作者单位
章泽军 中国地质大学地球科学学院湖北武汉430074 
张志 中国地质大学地球科学学院湖北武汉430074 
秦松贤 中国地质大学地球科学学院湖北武汉430074 
蔡雄飞 中国地质大学地球科学学院湖北武汉430074 
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摘要:
Pre-Sinian Basic Tectonic Framework of Northern South China and Its Evolution
      Pre-Sinian Paleoproterozoic material records available in northern South China suggest that the Yangtze plate had been prololly connected with cathaysia there at that time.The terminal Paleoproterozoic Lüliang movement was a prelude to tectonic movement in South China.This movement gave rise to paleo-islands represented by the Longquan paleo-island in Zhejiang and Xinzi paleo-island in Jiangxi,which were later overlain unconformably by Mesoproterozoic sediments.Geological and paleomagnetic evidence indicates that South China broke up into the Yangtze plate and Cathaysian plate in or before the middle-late Mesoproterozoic.The two plates have characteristics of different styles of movement.During 1 100 to 800 Ma,amalgamation and collision between the Cathaysian plate and Yangtze plate were completed.The Jinning movement,which is considered to be equivalent to the Greenville orogeny,marks the end of the evolution of the pre-Sinian basic tectonic framework of South China.
ZHANG Ze-jun,ZHANG Zhi,QIN Song-xian,CAI Xiong-fei.2003.Pre-Sinian Basic Tectonic Framework of Northern South China and Its Evolution[J].Acta Geoscientica Sinica,24(3):197-204.
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