| 富蕴地震断裂带南部结构特征 |
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| 引用本文： | 柏美祥.富蕴地震断裂带南部结构特征[J].内陆地震,2003,17(1):11-19. |
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| 作者姓名： | 柏美祥 |
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| 作者单位： | 新疆防御自然灾害研究所,新疆,乌鲁木齐,830011 |
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| 摘 要： | 富蕴地震断裂带南段主体走滑段多为正走滑断层，呈右行右阶或左阶排列。末端破裂段多不连续，呈弧形或左阶排列，部分沿支断层展布。
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| 关 键 词： | 地震断裂带 正走滑断层 断裂结构 地质构造 |
| 文章编号： | 1001-8956(2003)01-0011-09 |
| 修稿时间： | 2002年12月3日 |
STRUCTURAL FEATURES OF THE SOUTH SEGMENT OF THE FUYUN,XINJIANG,EARTHQUAKE FAULT ZONE |
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| BAI Mei,xiang.STRUCTURAL FEATURES OF THE SOUTH SEGMENT OF THE FUYUN,XINJIANG,EARTHQUAKE FAULT ZONE[J].Inland Earthquake,2003,17(1):11-19. |
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| Authors: | BAI Mei xiang |
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| Abstract: | The south segment of the Fuyun,Xinjiang,earthquake fault zone was divided into two parts:main strike slip segment and ended fracture segment.In the main strike slip segment there are many nomal strike slip faults distributed in right handed,right stepped or left stepped form.The ended fracture segment is much discontinuous, arranged in arcuate or left stepped form, and part spreads out along the branch fault. |
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| Keywords: | Earthquake fault zone Fault structure Qinghe |
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