| 论新疆深大断裂特征与地震的关系(3) |
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| 引用本文： | 宋和平.论新疆深大断裂特征与地震的关系(3)[J].内陆地震,2006,20(3):198-210. |
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| 作者姓名： | 宋和平 |
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| 作者单位： | 新疆维吾尔自治区地震局,新疆,乌鲁木齐,830011 |
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| 摘 要： | 北天山山前地带是构造运动十分强烈的地区,褶皱断裂等构造现象十分发育,这里曾发生过多次中强破坏性地震。由于受区域构造长期作用的影响,在北天山山前地区逐步发育形成了多排褶皱背斜及活动断裂,且运动方式具有独特性。该区域作为推覆逆冲的典型地区,其研究成果具有代表性和普遍性。
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| 关 键 词： | 北天山褶皱带 山前坳陷 博格达推覆构造 褶皱背斜 |
| 文章编号： | 1001-8956（2006）03-0198-13 |
| 收稿时间： | 2006-03-27 |
| 修稿时间： | 2006-06-19 |
THE RELATION BETWEEN CHARACTERISTICS OF DEPTH AND BIG FAULTS IN XINJIANG AND EARTHQUAKE |
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| SONG He-ping.THE RELATION BETWEEN CHARACTERISTICS OF DEPTH AND BIG FAULTS IN XINJIANG AND EARTHQUAKE[J].Inland Earthquake,2006,20(3):198-210. |
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| Authors: | SONG He-ping |
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| Institution: | Earthquake Administration of Xinjiang Uygur Autonomous Region, Urumqi 830011, Xinjiang, China |
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| Abstract: | The tectonic motion is very intense in front belt of north Tianshan mountain,drape fault and so on very develop,and there occurred many times destruct earthquakes.Under the effect of regional tectonics,there develop many raws drape anticline and active fault in the front of mountain,and they have especial motion fashion.The region is typical overriding obduction region,and the reseach results have representative and catholicness. |
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| Keywords: | Drape belt of north Tianshan mountain Sunken in front of mountain Bogeda overriding tectonics Drape acticline |
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