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尼勒克地震滑坡的统计分析及初步研究
引用本文:尹光华,李军,张勇,杨章.尼勒克地震滑坡的统计分析及初步研究[J].内陆地震,2001,15(1):56-63.
作者姓名:尹光华  李军  张勇  杨章
作者单位:新疆维吾尔自治区地震局,
摘    要:利用野外考察资料,对1812年新疆尼勒克地震的滑坡进行了统计分析和研究,认为尼勒克地震是一个典型的倾滑型地震,产生的地表破坏主要是地震滑坡,而且滑坡规模大,数量多,分布集中,其规模和分布密度与烈度成正比,有由震中向外变小、变稀的特点。

关 键 词:滑坡  倾滑型地震  天山地区  新疆  分布规模  地震烈度
文章编号:1001-8956(2001)01-0056-08
修稿时间:2000年5月19日

STATISTICAL ANALYSIS AND RESEARCH OF LANDSLIDES CAUSED BY NILEKE EARTHQUAKE
YIN Guang hua,LI Jun,ZHANG Yong,YANG Zhang.STATISTICAL ANALYSIS AND RESEARCH OF LANDSLIDES CAUSED BY NILEKE EARTHQUAKE[J].Inland Earthquake,2001,15(1):56-63.
Authors:YIN Guang hua  LI Jun  ZHANG Yong  YANG Zhang
Abstract:Based on the investigation data in field, statistical analysis and preliminary research on the landslides caused by 1812 Nileke, Xinjiang, earthquake were conducted. It is thought that Nileke earthquake is typically a dip slip type shock, the surface damage caused by which are main landslides. The landslides are large in scale, many in quantity, concentrated in distribution, with the feature that its scale and distributional density is in direct proportion to the intensity of the quake from the outside to the epicenter.
Keywords:Earthquake landslide  Dip  slip  type earthquake  Tianshan area  Nileke of Xinjiang
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