烃汞气体测量法在中非沉积型铜矿的找矿可行性研究
黄学强1(
), 陈远荣2, 吴二3, 刘峰1, 卢安宁1
), 陈远荣2, 吴二3, 刘峰1, 卢安宁1
The feasibility of applying hydrocarbon-mercury gas measurement method in the prospecting of sedimentary copper deposits in Central Africa
HUANG Xue-Qiang1(), CHEN Yuan-Rong2, WU Er3, LIU Feng1, LU An-Ning1
), CHEN Yuan-Rong2, WU Er3, LIU Feng1, LU An-Ning1
图4. 马本德矿区P2线地质—烃类异常剖面
1—冰川混积岩(小砾岩);2—白云岩化砂岩、粉砂岩或页岩;3—罗恩群(R3)白云岩、白云岩化粉砂岩;4—铜矿体;5—实测/推测地质界线;6—断裂
Fig.4. Geological hydrocarbon anomaly profile of P2 in Mabende-mining area
1—glacial migmatite (small conglomerate);2—dolomitized sandstone, siltstone or shale;3—Roan group (R3) dolomite, dolomitized siltstone;4—copper orebody;5—measured/inferred geological boundary;6—fault
