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渭河断裂带古地震研究
引用本文:师亚芹,李晋,冯希杰,戴王强,任隽,李晓妮,窦玛丽.渭河断裂带古地震研究[J].地震地质,2007,29(3):607-616.
作者姓名:师亚芹  李晋  冯希杰  戴王强  任隽  李晓妮  窦玛丽
作者单位:陕西省地震局,西安,710068
基金项目:国家发改委发改投资项目
摘    要:史料记载和涵洞路槽开挖表明,在距今9110a以来渭河断裂带窑店—张家湾段曾发生1次历史地震、3次古地震事件。其中历史地震即第Ⅳ期地震的发震时间在公元1487—1568年之间;事件Ⅰ为距今(9110±90)a,事件Ⅱ和事件Ⅲ距今时间不详。第Ⅰ,Ⅱ,Ⅲ期地震事件的同震垂直位移量分别为0.5,0.5,0.2m。涵洞路槽开挖也表明,渭河断裂窑店—张家湾段为全新世活动断裂

关 键 词:渭河断裂带  古地震  同震位移  探槽
文章编号:0253-4967(2007)03-0607-10
收稿时间:2007-09-13
修稿时间:2006-07-05

THE STUDY OF PALEOEARTHQUAKE ON THE WEIHE FAULT ZONE
SHI Ya-qin,LI Jin,FENG Xi-jie,DAI Wang-qiang,REN Jun,LI Xiao-ni,DOU Ma-li.THE STUDY OF PALEOEARTHQUAKE ON THE WEIHE FAULT ZONE[J].Seismology and Geology,2007,29(3):607-616.
Authors:SHI Ya-qin  LI Jin  FENG Xi-jie  DAI Wang-qiang  REN Jun  LI Xiao-ni  DOU Ma-li
Abstract:Weihe Fault is an important buried fault in Weihe basin.The predecessors have investigated the location and activity of the fault from various points of view,but up to now,the level of researches on the precise location and activity for the fault is still very low.There are few strata profiles of late Pleistocene which are found to be offset by the fault zone.Especially,it is still unknown whether the Weihe Fault was active in Holocene and there were paleoseismic events occurring on it.It is indicated from
Keywords:Weihe Fault zone  paleoearthquake  coseismic displacement  exploratory trench
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