摘要
通过物化探异常解释,区内激电异常幅值较低,且不呈规模分布,均未发现局部低阻中极化富集体。与矿区周边铅锌矿对比,区内成矿地层条件较差,主要原因是区内出露地层较新。根据化探异常推断,区内自地表以下500m范围内,存在铅锌矿(化)体的可能性较小。
Through the interpretation of geophysical and geochemical anomalies, the magnitude of the IP anomaly in the region is low, and it is not the size distribution. Compared with the lead-zinc deposits in the mining area, the formation conditions are poor in the area, the main reason is that the exposed strata in the area are relatively new. According to the geochemical anomaly, the possibility of the existence of lead-zinc ore (500m) in the area below the surface of the area is small.
出处
《世界有色金属》
2017年第5期164-166,共3页
World Nonferrous Metals
基金
基金项目:黔南科合农字(2015)4号
关键词
三都县三洞
铅锌矿矿
地质特征
物化探异常
three holes in Sandu County
lead-zinc deposit
geological characteristics
geochemical exploration anomaly