Correlation between Rimjingang belt and Dabie-Sulu orogenic belt  

作　　者：KIM Byongsong LIU Yongjiang LI Weimin LIANG Dojun KIM Myonghak CHAE Yongsik 

机构地区：[1]College of Earth Sciences, Jilin University, Changchun 130061, China [2]Department of Resources Exploration Engineering, KimChaek University of Technology, Pyongyang, DPR Korea [3]Department of Geology, Kim ll Sung University, Pyongyang, Korea [4]Department of Geological Exploration, Sariwon Geological University, Sariwon , DPR Korea

出　　处：《Global Geology》2012年第2期97-104,共8页世界地质（英文版）

摘　　要：The Dabie-Sulu orogenic belt in central-eastern China is considered as a high-pressure and ultrahighpressure metamorphic belt that demensions are comparatively large,and formed as a result of the collision of Sino-Korean and Yangtze cratons in eastern China. After continuous discoveries of high-pressure and ultra-high pressure metamorphic assemblages in the Dabie-Sulu area,the issue of the Dabie-Sulu orogenic belt extending eastward to the Korean Peninsula has been paid attentions widely. The discoveries of eclogites in the Hongsoeng area,the middle-western Korean Peninsula gives rise to the debate on the tectonic affiliations of the southern massifs. Although the Rimjingang belt in the Korean peninsula has been well investigated,the relation and comparative study to the Dabie-Sulu orogenic belt are lacking of detail work. In this paper,on the basis of informations and results of our previous works,some new contrastive considerations on the correlation between the Dabie-Sulu orogenic belt in central-eastern China and Rimjingang belt in the Korean Peninsula have are provided.The Dabie-Sulu orogenic belt in central-eastern China is considered as a high-pressure and ultrahighpressure metamorphic belt that demensions are comparatively large, and formed as a result of the collision of Si- no-Korean and Yangtze cratons in eastern China. After continuous discoveries of high-pressure and ultra-high pressure metamorphic assemblages in the Dabie-Sulu area, the issue of the Dabie-Sulu orogenic belt extending eastward to the Korean Peninsula has been paid attentions widely. The discoveries of eclogites in the Hongsoeng area, the middle-western Korean Peninsula gives rise to the debate on the tectonic affiliations of the southern massifs. Although the Rimjingang belt in the Korean peninsula has been well investigated, the relation and comparative study to the Dabie-Sulu orogenic belt are lacking of detail work. In this paper, on the basis of in- formations and results of our previous works, some new contrastive considerations on the correlation between the Dabie-Sulu orogenic belt in central-eastern China and Rimjingang belt in the Korean Peninsula have are provided.

关 键 词：Korean Peninsula Rimjingang belt Dabie-Sulu orogenic beh Rimjin Group structural characteristics 

分 类 号：P542[天文地球—构造地质学] Q959.837[天文地球—地质学]