摘要
江西省安福县浒坑钨矿床位于武功山穹隆花岗岩伸展构造的花岗变质核杂岩内,是一个大型石英脉型中—高温热液黑钨矿床。论文主要基于浒坑钨矿床近年来勘查成果和采矿实践开展分析研究,认为该矿床受地层、岩浆岩、构造联合控制,并提出了该矿床的找矿方向。
Hukeng tungsten deposit in Anfu County,Jiangxi Province is located in the granite metamorphic core complex of the extensional structure of Wukongshan dome granite.It is a large quartz vein type medium-high temperature hydrothermal wolframite deposit.The paper is mainly based on the exploration results and mining practice of keng tungsten deposit in recent years,believing that the deposit is jointly controlled by stratum,magma rock and structure,and the prospecting direction of the deposit is proposed.
作者
欧阳淇生
张连湘
余光模
OUYANG Qi-sheng;ZHANG Lian-xiang;YU Guang-mo(Jiangxi Nonferrous Geological and mineral exploration and Development Institute,Nanchang 330001,China;Jiangxi natural resources development center,Nanchang 330001,China)
出处
《世界有色金属》
2021年第21期59-60,共2页
World Nonferrous Metals
关键词
浒坑地区
钨矿
控矿因素
找矿方向
Hukeng area
Tungsten ore
Mining control factors
the prospecting prediction