CAJ | 학술논문

为查明高放废物处置库深部地质特征，采用大地电磁法、可控源音频大地电磁法以及高精度磁法进行综合地球物理勘探与资料解译，得到6条测线的综合地球物理成果解译图。根据成果解译图的异常特征，推断出研究区花岗岩体受南北两侧两条近东西向断裂F1、F2控制，破碎带分布较宽，断层充填高热蚀变物质，岩体内部无明显断层发育。
위사명고방폐물처치고심부지질특정，채용대지전자법、가공원음빈대지전자법이급고정도자법진행종합지구물리감탐여자료해역，득도6조측선적종합지구물리성과해역도。근거성과해역도적이상특정，추단출연구구화강암체수남북량측량조근동서향단렬F1、F2공제，파쇄대분포교관，단층충전고열식변물질，암체내부무명현단층발육。
To find out the deep geological characteristics of high -level radioactive waste disposal repository .U-sing magnetotelluric method ,the controlled source audio magnetotelluric method and high -precision magnetic method for comprehensive geophysical prospecting and data interpretation ,get 6 lines'results interpretation chart of integrated geophysical .According to the anomalous characteristics of the results interpretation chart , deduced that the granite controlled by both the north and south sides of two near ? EW trending faults F 1 and F2 ,with a wide distribution in fracture zones ,and fault filling heat alteration material .The granite rock mass have no obvi-ous internal fault development .