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《Chinese Journal of Geophysics》 1997-01
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INVESTIGATION ON MT DATA ALONG YANGGAO RONGCHENG PROFILE BY TWO-DIMENSIONAL INVERSION

ZHAO GUO-ZE; LIU TIE-SHENG; JIANG ZHAO; TANG JI; XU CHANG-FANG;ZHAN YAN; BAI DENG-HAI; LIU GUO-DONG(Institute of geology. State Seismological Bureau, Beijing 100029,Chia)  
A new MT inversion method-rapid two-dimensional magnetotelluric inversion iswell applied in the interpretation of the data observed along the profile from Yanggao inShanxi province to Rongcheng in Hebei province. Inversion results show that electricity structure in the shallow depth can be compared with geological set. A low resistivity zoneoccures in the middle and lower crust and appeares inhomogenely. It can be divided intothree sections along the profile. The depth of the low resistivity zone in the upper mantledecreases from NW end of the profile (about 150km or more) to SE end (less than100km). A steep rising section of its depth along profile exists under the high gradient ofthe tremendous gravity anomaly which passed througt east China. Several major faultscrossed this profile are indicated by the large resistivity contrasts.
【Fund】: 国家“八五”科技攻关项目;;国家自然科学基金;;地震科学联合基金
【CateGory Index】: P318
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