| Late-Quaternary Movement Along the Sertengshan Piedmont Fault and a Model for Segmentation of Its Rupture |
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| 作者姓名： | Chen Lichun |
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| 作者单位： | InstituteofGeologyChinaEarthquakeAdministration,Beijing100029,China |
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| 基金项目： | TheresearchwassupportedunderaprojectofStateKeyBasicResearchandDevelopmentPlan (G1 9980 4 0 7)，China . |
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| 摘 要： | Analysis and study of the geometrical structure of the fault, tectonic features of late-Quaternary movement, paleoseismic activity, and structural characteristics of boundaries between segments of the Sertengshan piedmont fault permitted us to preliminarily determine the following 4 active segments of the fault: the Wujiahe segment (from Dongwugai Gully to Dahoudian Village),Wujumengkou-Dongfeng Village segment (from Dahoudian to Delingshan), Dashetai segment (from Delingshan to Xiaoshetai Gully mouth), and the Ulan Hudong segment (from Xiaoshetai Gully mouth to Tailiang). The boundaries between them are the Dagoudian mountain spur,the Delingshan Mountain spur and the step zone at Xiaoshetai Gully mouth, respectively. The segments are independent for seismic activity. However, it is possible that joint ruptures between Wujiahe and Wujumengkou-Dongfeng Village segments and between Dashetai and Ulan Hudong segments may occur.
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| 关 键 词： | 活性断层 分割 几何构造 边界线 |
Late-Quaternary Movement Along the Sertengshan Piedmont Fault and a Model for Segmentation of Its Rupture |
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| Chen Lichun.Late-Quaternary Movement Along the Sertengshan Piedmont Fault and a Model for Segmentation of Its Rupture[J].Earthquake Research in China,2004,18(1):67-78. |
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| Authors: | Chen Lichun |
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| Affiliation: | Chen Lichun,Ran Yongkang,Yang Xiaoping and Guo WenshengInstitute of Geology,China Earthquake Administration,Beijing 100029,China |
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| Abstract: | Analysis and study of the geometrical structure of the fault, tectonic features of late Quaternary movement, paleoseismic activity, and structural characteristics of boundaries between segments of the Sertengshan piedmont fault permitted us to preliminarily determine the following 4 active segments of the fault: the Wujiahe segment (from Dongwugai Gully to Dahoudian Village), Wujumengkou Dongfeng Village segment (from Dahoudian to Delingshan), Dashetai segment (from Delingshan to Xiaoshetai Gully mouth), and the Ulan Hudong segment (from Xiaoshetai Gully mouth to Tailiang). The boundaries between them are the Dagoudian mountain spur, the Delingshan Mountain spur and the step zone at Xiaoshetai Gully mouth, respectively. The segments are independent for seismic activity. However, it is possible that joint ruptures between Wujiahe and Wujumengkou Dongfeng Village segments and between Dashetai and Ulan Hudong segments may occur. |
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| Keywords: | Sertengshan piedmont fault Active fault Segmentation Paleoseismicity |
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