| 富蕴地震断裂带北部细部结构特征 |
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| 引用本文： | 柏美祥.富蕴地震断裂带北部细部结构特征[J].内陆地震,2001,15(2):97-103. |
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| 作者姓名： | 柏美祥 |
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| 作者单位： | 新疆维吾尔自治区地震局, |
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| 摘 要： | 以8级地震时的水平位移作为地震断裂带分段依据，富蕴地震断裂带北部引张段长17km，而且水平位移不明显。富蕴地震断裂带的主体走滑段水平位移显著，除大震时的水平位移外，发震构造具多期次活动特征。
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| 关 键 词： | 水平位移 细部结构 地震断裂带 发震构造 |
| 文章编号： | 1001-8956（2001）02-0097-07 |
DETAILED STRUCTURAL FEATURES IN THE NORTH OF FUYUN EARTHQUAKE FAULT ZONE |
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| BAI Mei,xiang.DETAILED STRUCTURAL FEATURES IN THE NORTH OF FUYUN EARTHQUAKE FAULT ZONE[J].Inland Earthquake,2001,15(2):97-103. |
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| Authors: | BAI Mei xiang |
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| Abstract: | Based on the horizontal displacements formed in Fuyun M=8 earthquake, the Fuyun seismic fault zone was divided into two parts:northern extension segment and main strike slip segment. The northern extension segment is as long as 17 km, without obvious horizontal displacement. In the main strike slip segment there is notable horizontal displacement, which is the result of many times of seismic activities. |
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| Keywords: | Horizontal displacement Detailed structure Seismic fault zone Fuyun |
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