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《JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY》 2000-02
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THE ESTABLISHMENT AND TECTONIC EVOLUTION OF PROTEROZOIC OROGENIC BELT IN THE NORTH MARGIN OF NORTH CHINA PLATE

LIU Zheng_hong, LIU Ya_qin, FENG Ben_zhi (Changchun University of Science and Technology, Changchun 130026, China)  
There is the collision orogenic belt which was developed in late middle Proterozoic era, in north margin of North China plate. The belt extends from Langshan in Inner Mongolia to Western Liaoning province and Eastern Jilin province. Its length is over 2 000 km. A variety of metamorphic sedimentary rocks, volcanic rocks and plutonic rocks were developed in this tectonic belt. This significant tectonic belt was formed by the collision between Siberia plate and North China plate in about 1.0 Ga. This tectonic event was a part of Rodinia super continent convergence event.It is clear that Siberia platform connected with North China platform during period of Rodinia supercontinent.
【Fund】: 国家自然科学基金项目!(4 9872 0 71 );;; 国土资源部地调局内蒙古大青山地区 6幅 1∶ 5万区调项目!(0 1 992 0 90 3 1 )
【CateGory Index】: P542.4
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