高放废物处置库深部地质特征研究  

Study on the Deep Geological Characteristics of High-Level Radioactive Waste Disposal Repository

作　　者：吴赞华[1,2] 董湘龙[3] 李忠权[1] 时燕华 邓晓颖 

机构地区：[1]成都理工大学,成都610059 [2]江西省核工业地质局,南昌330046 [3]核工业二三〇研究所,长沙410011 [4]核工业西藏地质调查院,成都610081

出　　处：《核电子学与探测技术》2014年第3期296-300,368,共5页Nuclear Electronics & Detection Technology

基　　金：国家自然科学重点基金(41030426);国家“十二五”科技重大专项(2011ZX05004-005-01);四川省构造地质重点学科(SZD0408)联合资助

摘　　要：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。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＆#39;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 .

关 键 词：高放废物 地质特征 地球物理 

分 类 号：P542.5[天文地球—构造地质学]