摘要
本文在阐述了仙水沥矿区基本地质特征、1∶1万土壤异常特征及可控源音频大地电磁法测深(CSAMT)特征的基础上,分析了锡钨多金属矿体特征,初步认为该矿床成因为岩浆期后高-中温热液裂隙充填交代矿床。
On the basis of expounding the basic geologicalcharacteristics,1:10000 soil anomaly characteristics andCSAMT characteristics of Xianshuili mining area and analyzing the characteristics of Sn-W polymetallic ore body,it is preliminarily considered that the deposit is formed because of post-magmatic high-to medium-temperature hydrothermal fissure filling metasomatic deposit.
作者
汤琳
赵新胤
TANG Lin;ZHAO Xin-yin(Nonferrous metals geological bureau of Guangdong privince 931 battalion,Shantou 515041,China)
出处
《世界有色金属》
2022年第16期63-65,共3页
World Nonferrous Metals
关键词
仙水沥
地质特征
土壤异常
CSAMT
成因类型
Xianshuili
geological characteristics
soil anomaly
CSAMT
genetic industry type
