| The Feature of Segmentation Activity on the Northern Segment of the Anninghe Fault Zone Since Late Pleistocene |
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| 作者单位： | Tang Rongchang，Qian Hong，Huang Zuzhi，Wen Dehua，Wu Xianguo，Cai Changxing and Tian Hong Seismological Bureau of Sichuan Province，Chengdu 610041，China |
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| 摘 要： | Based on fault geometric features,composite pattern,faulting land-forms and seismic data,this paper discussed the activity behavior along the northern segment of the Anninghe fault(from Xichang to Shimian)since the Late Pleistocene.The fault can be divided into three active segments by discrepancies of their activity:the segment from Xichang to Mianning,the segment from Mianning to Zimakua,and the segment from Zimakua to Tianwan.The southern segment has the background of occurrence of great earthquakes,but the middle and the northern segments can generate strong and moderate events respectively.According to the features of quartz from fault gouges by scanning electron microscopy(SEM),this paper discussed the movement features along the fault and indicated the stick-slipping feature on the segment from Xichang to Zimakua,the creeping feature on the segment from Jiziping to Tianwan and the transitional feature on the segment in between.
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The Feature of Segmentation Activity on the Northern Segment of the Anninghe Fault Zone Since Late Pleistocene |
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| Tang Rongchang,Qian Hong,Huang Zuzhi,Wen Dehua,Wu Xianguo,Cai Changxing and Tian Hong Seismological Bureau of Sichuan Province,Chengdu ,China. The Feature of Segmentation Activity on the Northern Segment of the Anninghe Fault Zone Since Late Pleistocene[J]. Earthquake Research in China, 1994, 0(4) |
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| Authors: | Tang Rongchang Qian Hong Huang Zuzhi Wen Dehua Wu Xianguo Cai Changxing Tian Hong Seismological Bureau of Sichuan Province Chengdu China |
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| Affiliation: | Tang Rongchang,Qian Hong,Huang Zuzhi,Wen Dehua,Wu Xianguo,Cai Changxing and Tian Hong Seismological Bureau of Sichuan Province,Chengdu 610041,China |
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| Abstract: | Based on fault geometric features,composite pattern,faulting land-forms and seismic data,this paper discussed the activity behavior along the northern segment of the Anninghe fault(from Xichang to Shimian)since the Late Pleistocene.The fault can be divided into three active segments by discrepancies of their activity:the segment from Xichang to Mianning,the segment from Mianning to Zimakua,and the segment from Zimakua to Tianwan.The southern segment has the background of occurrence of great earthquakes,but the middle and the northern segments can generate strong and moderate events respectively.According to the features of quartz from fault gouges by scanning electron microscopy(SEM),this paper discussed the movement features along the fault and indicated the stick-slipping feature on the segment from Xichang to Zimakua,the creeping feature on the segment from Jiziping to Tianwan and the transitional feature on the segment in between. |
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| Keywords: | Anninghe fault Faulting landform Most recently active surface fault Stick slipping Creeping |
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