Fankou

基本解釋

Fankou Pb-Zn deposit is a submarinehydrothermal spring effusion type ore deposit, which occurred in upper Paleozoic carbonaterock formation.
凡口鉛鋅礦床是發(fā)育于上古生界碳酸鹽巖建造中的海底熱泉噴溢礦床。
The environmental effect of typha latifolia on disposal of sewage and tailing of Fankou lead zinc mine is described.
介紹了香蒲植物在凡口鉛鋅礦污水處理以及尾礦治理中的環(huán)保作用。
The form, distribution and emplacement are controlled by many factors in Fankou Pb-Zn ore deposit.
(4)礦區(qū)鉛鋅硫化物礦床的形成、分布和礦體具體定位同時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.
研究對象主要有廣東凡口和樂昌鉛鋅礦尾礦；
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，凡口鉛鋅礦與韶關冶煉廠實行強強聯(lián)合，組建為廣東韶關嶺南鉛鋅集團公司。