ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
华北地台东缘的印支运动烙印——来自大连地区的构造形变信息
  
关键词:Dalian area  structural deformation  Indosinian orogeny
基金项目:地质调查项目“大连市等六幅 1∶5万区域地质调查”
作者单位
邴志波 中国地质调查局沈阳地质矿产研究所辽宁沈阳110032 
王宗秀 中国地质科学院地质力学研究所北京100037 
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摘要:
Indosinian Orogeny in the Eastern Margin of North China Platform:Tectonic Deformation in Dalian Area
      As a typical area of intense deformation on thestable platform, Dalian area has been subjected to multi-phase intense deformation events since Mesozoic. Due to violent structural reformation and superimposed deformation, its crustal structure is very complicated. The NS-trending shear traction deformationis the largest and most influential structural deformation in the area, forminggigantic recumbent folds and overturned folds and resulting in large-scale stratigraphic overturning. In this paper, the authors have studied the NS-trendingshear traction deformation through detailed geological investigation and structural analysis, and determined the age of this deformation. It is considered that the post-Indosinian orogeny is the fundamental structural event of the fold-structure framework in Dalian area. The large-scale intraplate deformation is an intracontinental deformation effect of the continent-continent collision between Yangtze plate and Sino-korean plate.
BING Zhi-bo,WANG Zong-xiu.2004.Indosinian Orogeny in the Eastern Margin of North China Platform:Tectonic Deformation in Dalian Area[J].Acta Geoscientica Sinica,25(5):555-560.
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