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《JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY》 1996-01
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THE SOUTHWARD MOVEMENT IN PALAEOZOIC ERA FROM NEW PALAEOMAGNETIC DATA OF NORTH QILIAN TERRANE

Yang Huixin; Dong Xuebin; Li Pengwu(Changchun University of Earth Sciences, Changchun 130026)  
Through palaeomagnetic study of North Qilian terrane tectonics in geoscience transection from Golmud to Ejina banner,eight new palaeomagnetic data of palaeozoic and Mesozoic Era are obtained and it is indicated that North Qilian had been located in low latitude area North latitude (10°~17°degrees)during palaeozoic. In palaeozoic,terrane showed an episode of evident southward movement,which began at early silurian and ended at early carboniferous.Up to late permian,the terrane began to return.The amplitude of southern movement is about 5. 5 degrees.It may be relative to extension of the primitive continental crust in North Qilian area in middle ordovician and its filing and welding of later period.
【Fund】: 格尔木-额济纳旗地学断面综合研究"项目自然科学基金重
【CateGory Index】: P318.4
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