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《JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY》 1995-04
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UPLIFT BEDDING -DELAMINATION STRUCTURE IN CONTINENTAL OROGEN ──a new model of pre-orogenic extensional tectonics

Yang Zhensheng;Li Sanzhong;Liu Yongjiang(changchun Uni.of Earth Sci.,Changchun 130026)  
Based on the detailed study on orogenic belts, a new structual model,thelocal uplift bedding-delamination structural series(UBDSS),is proposed in this paper.The pre-orogenic extensional tectonics probably causes such structural type whichconsists of three parts:core,cover and contact plane,It is very different frommetamorphic core complex. Because the appearance is similar to metamorphic corecomplex, it is easily misregarded as metamorphic core complex. The uplift bedding-delamination structure is very important in the structural succession of orogenic beltbecause of its special forming stage and structural architecture. The identification anddetermination of UBDSS have important significance for the study of orogenic belt.UBDSS is normally superposed by shortening structures so that its primary appearnce isuncertain. However, the uplift bedding-delamination structure could be generallyobserved in the anticlinoria belts,The study of uplift bedding-delamination structure issignificant to the research of orogenic tectonics,stratigraphy,metamorphism anddetermination,and so on.
【CateGory Index】: P524.2
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