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 Il Sung University��Pyongyang��Korea; 4�� Department of Geological Exploration��Sariwon Geological University��Sariwon��DPR Korea

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��