摘要
川口三角潭钨矿床与华南众多同类型矿床有别 ,矿床不具“五层楼”特征 ,而具逆向分带现象 ,是一个受岩浆岩和断裂构造双重控制 ,矿液致裂作用形成的高—中温 ,以黑钨矿为主的钨—多金属矿床。
Sanjiaotan Tungsten deposit of Chuankou, different from many other ore deposits of this type in South China,with the phenomenon of reverse zoning and without the feature of “Five-storey”,is a high-mesothermal temperature tungsten polymetallic ore deposit dorninated by wolframite, which is formed by hydrofract uring and controlled by both magma rock and fracture strutures.
出处
《矿产与地质》
2000年第5期285-288,共4页
Mineral Resources and Geology
基金
国家自然科学基金项目!(编号 4 9772 152 )
关键词
矿液致裂
矿床成因
逆向分带
钨矿床
岩浆岩
断裂构造
Hydrofacturing
Genesis of ore deposits
Reverse zoning
Sanjiaotan
Tungsten Deposit
