干旱荒漠区综合物化探方法寻找铜多金属矿

龚胜平, 陆桂福, 席明杰, 马生明, 苏文利

The application of integrated geophysical and geochemical methods to the prospecting of copper polymetallic deposits in the arid desert area

GONG Sheng-Ping, LU Gui-Fu, XI Ming-Jie, MA Sheng-Ming, SU Wen-Li

图2 激电中梯测量视电阻率(a)与视充电率(b)等值线平面 a—视电阻率平面图;b—视充电率平面图;构造为地质实测,地球物理色标仅应用于调查区范围内,地质背景图例见图1,图3~6同

Fig.2 Contour maps of the apparent resistivity(a) and apparent chargeability(b) of the TDIP survey a—the plan view of apparent resistivity;b—the plan view of apparent chargeability;the fracture is measured by geological means, and the geophysical color unit is only used in the survey area,the geological legend is shown in Fig.1,and Fig.3~Fig.6 are the same