摘要
该金矿产于哀牢山构造带南段,矿床的形成与哀牢山的构造岩浆活动密切相关,本文通过对该矿床成矿地质背景、矿体特征、矿石特征、找矿标志进行分析研究,判断该矿床为一中低温热液型金矿,矿体多受断层破碎带或层间破碎带控制,通过该矿床成因研究,以期为后续勘查工作提供一定指导。
This gold mineral belongs to Ailaoshan tectonic belt in the southern section,the paper of the ore-forming geological background,geological characteristics,ore characteristics,prospecting signs were analyzed to determine if the deposit is an epithermal gold deposit in,ore and more by the fault fracture zone or interlayer fracture zone controlled by the deposit genesis study,in order to provide some guidance for future exploration work.
出处
《世界有色金属》
2016年第9S期61-62,共2页
World Nonferrous Metals
关键词
金矿床
地质特征
成因分析
云南
gold deposit
geological characteristics
genesis analysis
Yunnan
