摘要
研究区位于招平断裂带东侧。地层主要为古元古代荆山群和第四系,构造主要为NE、NEE向两组断裂。通过高精度磁测工作圈定一个磁异常,物探解译非矿致异常。通过土壤化学测量圈定3个综合异常和多个单元素异常,通过槽探、钻探对综合异常查证,证实是金矿体引起异常。建议对发现金矿体进行追索和控制,探求更多金金属量。
The study area is located on the east side of Zhaoping fault zone. The formation is mainly Paleoproterozoic Jingshan and quaternary structure, mainly for NE, NEE to two groups of faults. Through the soil chemical measurements delineated 3 integrated anomaly and multiple single element anomalies, by trenching and drilling for comprehensive anomaly verification, proved to be caused by abnormal ore body. It is suggested that the gold deposits should be controlled and controlled for more gold.
出处
《世界有色金属》
2017年第5期161-162,共2页
World Nonferrous Metals
关键词
金矿
地质特征
激电异常
土壤化探异常
Gold deposit
geological characteristics
IP anomaly
Geochemical anomaly