不同地质背景下EH-4的应用效果

李英宾, 李毅, 张占彬, 张伟

The application effect of EH-4 under different geological backgrounds

Ying-Bin LI, Yi LI, Zhan-Bin ZHANG, Wei ZHANG

图2 H15K01线(2008年AMT测量L02线)反演电阻率断面及地质推断解释 1—上白垩统二连组;2—下白垩统赛汉组;3—前白垩纪基底;4—砂岩;5—泥岩;6—角度不整合地质界线;7—岩相界线;8—推断的断裂构造

Fig.2 Inversion of resistivity profile and geological interpretation map of H15K01 line (2008 AMT surveying L02 line) 1—Erlian group of The upper Cretaceous; 2—the lower Cretaceous Saihan formation; 3—pre Cretaceous basement; 4—sandstone; 5—mudstone; 6—angle unconformity geological boundary; 7—facies boundary; fault 8—inference