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邢台震区地壳上地幔电性结构及其构造意义
引用本文:邓前辉,张木生.邢台震区地壳上地幔电性结构及其构造意义[J].地震地质,1997,19(2):60-163.
作者姓名:邓前辉  张木生
作者单位:国家地震局地质研究所
摘    要:用大地电磁测深(MT)方法在邢台地震区作了4条观测剖面,资料解释结果表明探测区地壳上地幔的电性结构主要特征为:震源区复杂,周边区简单;发震深度复杂,非发震深度简单;震源区电性突变,显示隐伏高角度断裂;高导层代表10km和20km深度的滑脱面;地幔上隆可能意味着地幔物质向上运移。这些观测结果对于了解测区构造背景、发震构造和深浅构造的关系有重要意义

关 键 词:大地电磁测深  电阻率  壳幔构造  邢台地震

GEOELECTRICAL STRUCTURE OF THE CRUST AND UPPLE MANTLE IN THE XINGTAI EARTHQUAKE AREA AND ITS TECTONIC IMPLICATIONS
Deng Qianhui,Zhang Musheng,Zhan Yan,Tang Ji,Zhao Guoze,Liu Tiesheng.GEOELECTRICAL STRUCTURE OF THE CRUST AND UPPLE MANTLE IN THE XINGTAI EARTHQUAKE AREA AND ITS TECTONIC IMPLICATIONS[J].Seismology and Geology,1997,19(2):60-163.
Authors:Deng Qianhui  Zhang Musheng  Zhan Yan  Tang Ji  Zhao Guoze  Liu Tiesheng
Abstract:Magnetotelluric (MT) sounding observations have been carried out along four profiles in the Xingtai earthquake area and its neighbouring regions. The results show characteristics of the geoelectrical structure of the crust and upper mantle for this region. The focal area looks like complex, while the surrounding area seems to be simple. The range of seismogenic depth is more complicated than the other depth range. Sharp changes of the electrical structure of the focal area indicate the hidden faults with st...
Keywords:Magnetotelluric sounding  Resistivity  Crust  mantle structure  Xingtai earthquake  
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