Fankou

基本解释

Fankou Pb-Zn deposit is a submarinehydrothermal spring effusion type ore deposit, which occurred in upper Paleozoic carbonaterock formation.
凡口铅锌矿床是发育于上古生界碳酸盐岩建造中的海底热泉喷溢矿床。
The environmental effect of typha latifolia on disposal of sewage and tailing of Fankou lead zinc mine is described.
介绍了香蒲植物在凡口铅锌矿污水处理以及尾矿治理中的环保作用。
The form, distribution and emplacement are controlled by many factors in Fankou Pb-Zn ore deposit.
(4)矿区铅锌硫化物矿床的形成、分布和矿体具体定位同时受多方面因素的控制。
Fankou and Lechang Pb/Zn mine tailings and Yunfu, Yingde and Yangchun pyrite mine spoils were studied.
研究对象主要有广东凡口和乐昌铅锌矿尾矿；
In July, 1997, Fankou Lead-Zinc Mine and Shaoguan Smelting Plant were practicing power-power association and jointly set up Guangdong Shaoguan Lingnan Lead-Zinc Group Company.
1997年7月，凡口铅锌矿与韶关冶炼厂实行强强联合，组建为广东韶关岭南铅锌集团公司。