1.
Characteristics of Strike-Slip Structures and Metallogenic Model of the Fankou Lead-Zinc Deposit,Guangdong Province
广东凡口铅锌矿床的走滑构造及成矿模式
2.
Concentrates Rule and Ore Body Predicting of Fankou Lead-Zinc Mine,Guangdong
广东凡口铅锌矿床成矿地质特征及资源预测
3.
Metallogeny of Fankou Superlarge Pb-Zn Ore Field, Guangdong Province;
广东凡口超大型铅锌矿田成矿学研究
4.
A genetic mineralogical study of sphalerite in the Fankou Pb-Zn ore district
凡口铅锌矿区闪锌矿的成因矿物学特征研究
5.
Analysis of Dilation and Loss Ratio in Fankou Pb-Zn Mine
凡口铅锌矿采场贫化率与损失率分析
6.
The Research of the Efficiency of Grinding Classification in Fankou Mine;
提高凡口铅锌矿二段磨矿分级效率研究
7.
Research and Practice on Colligate Recovery Silvery Resource from the Fan Kou Lead Zinc Ore;
凡口铅锌矿银矿物资源综合回收的研究与实践
8.
Heavy Metal Behavior During the Oxidation of the Fankou Pb-Zn Mine Tailings in Guangdong Province of China: Implications for Environmental Remediation at Mining Impacted Sites;
粤北凡口铅锌矿尾矿风化作用及其环境效应
9.
Assessment and Improvement of the Mine Ventilation System of Fankou Lead & Zime Mine;
凡口铅锌矿矿井通风系统评价与改造研究
10.
STUDY ON VARYING-COLOUREL BLENDE IN A LEAD-ZINC ORE DEPOSIT IN GUANGDONG
广东某铅锌矿床中不同颜色闪锌矿的研究
11.
Research on the Key Technologies of Mud Making and Tailing Releasing of Vertical Sand Tank in Fankou Lead-Zinc Mine
凡口铅锌矿立式砂仓造浆与放砂关键技术研究
12.
The Geological Characteristics of Yinshanli Pb-Zn-Ag Deposit,Dapu County,Guangdong Province
广东大埔县银山里铅锌银矿区矿床地质特征
13.
Basic Studies and Industrial Practice of Treatment and Reuse of Wastewater of Fankou Mill;
凡口选矿回水中铅锌硫化矿浮选基础研究与工业实践
14.
Geological characteristics and prognosis of prospects of Jinkeng Cu-Sn-Pb-Zn deposit,Jiexi County,Guangdong Province
广东省揭西金坑铜锡铅锌矿区矿床地质特征与远景预测
15.
Laboratory Study of No 4 Gold Ore Body Mining by Leaching in Shuikoushan Lead and Zinc Mine
水口山铅锌矿4~#金矿体矿石室内试验
16.
Research on Ore Controlling Conditions in Fozichong Pb-Zn Ore Field, Guanxi;
广西佛子冲铅锌矿床的控矿条件研究
17.
The Study of Exploring Prediction in the Deep of Fozichong Pb-Zn Deposit, Guangxi;
广西佛子冲铅锌矿深部找矿预测研究
18.
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。