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《Journal of Zhejiang University(Natural Science)》 1993-02
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Paleomagnetic feafures of middlepaleozoic rocks from western Zhejiang and southern Anhui, Yangtze Plate

Wu Nengyou Fang Dajun Jin Guohai(Department of Earth Sciences)  
This paper describes the paleomagnetism on middle Paleozoic rocks from western Zhe-jiang and southern Anhui of the Yangtze Plate, South China. According to the remmanent magnetization it is revealed that natural remmanences from middle Paleozoic rocks were com-posee of two or three components isloated from stepwise demagnetized vectors. Stability testes,such as fold test, fabric tedt,ect. , indicate that characteristic remmanent magnetiza- tions were primary. The mean directions and their poles of relatded ages in middle Paleozoic for Yangtze Plate have been obtained by applying two-tier stazistics. The results show that the western Zhejiang and southern Anhui region remained in southern equatorian latitudes during early Paleozoic,but moved by large scale absoute anticlockwise rotation between middle Silurian and early to middle Devonian.
【Fund】: 国家自然科学基金(4880176)
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