1) Tudaban Pb-Zn deposit
土达坂铅锌矿
1.
Tudaban Pb-Zn deposit is located in the transition between Qilian orogen and Dunhuang block,and hosted at the 2nd member of the 2nd formation,Archean-Proterozoic Dunhuang group.
肃北县土达坂铅锌矿地处祁连造山带与敦煌地块的交接部位,太古宙—古元古代敦煌岩群第二岩组第二岩段是其主要赋存层位。
2) Arhada Pb-Zn deposit
阿尔哈达铅锌矿
1.
Arhada Pb-Zn deposit occurs mainly in cataclastic zone of Devonian System and ore bodies are dominated by blind ones in en echelon and locally cut with each other.
阿尔哈达铅锌矿主要产于泥盆系的NW向断裂破碎带中,矿体具雁行排列、局部交叉产出的特征,以盲矿体为主;成矿早期可能以岩浆热液(399~407℃)为主,而中、晚期的热液以大气降水或混合水(194~287℃)为主;硫分别来源于岩浆热液、沉积地层和大气降水;铅同位素测试结果则显示了成矿(岩)物质的混源特点。
2.
Arhada Pb-Zn deposit is located in strata of Devonian and Permian System near intermediate-acidic intrusive rocks and controlled by the NE fault-traversed sub-scale faults.
阿尔哈达铅锌矿产于中酸性岩体附近的泥盆系、二叠系中,受与NE向断裂贯通的成群(组)出现的次级断裂控制;矿体连续性较好,平面上呈透镜状,空间上呈柱状、似板状、透镜状,矿体为隐伏-半隐伏状,埋深不大;矿床属于中低温热液矿床。
3) Dasaituo Pb-Zn camp
达赛脱铅锌矿
1.
Regional structural analysis of Dongwuqi county and local structural analysis of Dasaituo Pb-Zn camp show that NEE structures are the main ore-controlling structure.
通过对东乌旗区域构造及达赛脱铅锌矿区构造带的分析,阐明了NEE向构造为达赛脱铅锌矿区的主要控矿构造。
4) soil polluted lead/zinc mine tailings
铅锌尾矿土壤
1.
Resistance and uptake of heavy metals by four herbaceous plants from soil polluted lead/zinc mine tailings;
四种草本植物对铅锌尾矿土壤重金属的抗性与吸收特性研究
5) Arhada Ag-Pb-Zn camp
阿尔哈达银铅锌矿床
6) soil polluted by lead/zinc mine tailings
铅锌尾矿污染土壤
1.
Resistance to and uptake of heavy metals by four herbaceous plants grown in the soil polluted by lead/zinc mine tailings;
4种草对铅锌尾矿污染土壤重金属的抗性与吸收特性
补充资料：哈达阳
“哈达阳”为达语，因村东有陡山，山崖之下有深水，达语称山崖下的深水为“哈地阿沿”，村名由此而得，以后演变为“哈达阳”，现在也有称“哈达彦”（“哈达沿”）。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条