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《地球科学》 1994-04
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Extensional Dongwu Movement in Western Margin of Yangtze Region

Liang Dingyi (China University of Geosciences, Wuhan 430074)Nie Zetong Song Zhimin (China University of Geosciences, Beijing 100083)  
Permian seismites are well - developed along the western margin of the Yangtze region. Their presence together with the extensional seismic unconformity have enabled the authors to determine their age and the existence of the Dongwu movement, and to demonstrate also that in the region concerned a significant extensional structural event had taken place by the end of the Palaeozoic. The multicyclothemic seismite, and "the orderly - disposed fossils within mixed deposits" are related to frequent normal faulting at submarine border. In the Muli area earthquakes, extensional depressions, and volcanism had persisted since the beginning of the Dongwu movement and resulted in ruptured depressions ( reaching its climax by Late Permian - Early Triassic),It is there that the Dongwu movement is practically a depression movement.
【Fund】: 地矿部行业基金(项目90027)资助
【CateGory Index】: P542
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