摘要
为了研究呼热郭勒沟钼多金属矿床成因,综合评价该区找矿潜力,从区域地质背景、物化探异常特征、矿床特征、矿石质量等方面进行了综合分析。结果表明:呼热郭勒沟铜多金属矿床成因类型为受断裂阻容富集的与隐伏花岗岩岩体侵入活动密切相关的热液—斑岩型矿床,深部具有较大的找矿潜力。
To study the genesis of Hureguolegou molybdenum polymetallic deposit,the prospecting potential of the area is comprehensively evaluated.The paper analyzes the regional geological background,geophysical and geochemical anomaly characteristics,deposit characteristics and ore quality.The results show that the genetic type of the Hureguolegou copper polymetallic deposit is a hydrothermal-porphyry deposit closely related to the intrusion activity of the concealed granite.It has a large potential for prospecting in the deep.
作者
周鹏
杜生鹏
ZHOU Peng;DU Shengpeng(The First Geological Exploration Institute of Qinghai Province,Ping’an,Qinghai 810600,China)
出处
《中国锰业》
2019年第5期68-74,共7页
China Manganese Industry
关键词
钼多金属矿
地质特征
矿床成因
找矿潜力
Molybdenum polymetallic ore
Geological Features
Mineral deposit cause
Prospecting potential
