1) 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。
2) Arhada Ag-Pb-Zn camp
阿尔哈达银铅锌矿床
4) Haarhadda iron deposit
哈尔哈达铁矿
1.
Haarhadda iron deposit is one of the most important Fe deposits in Inner Mongolia Province,it is found that the ore source beds lie in sericite-quartz schist-hosted rock section of the Ondor Sum Group Haarhadda Formation.
哈尔哈达铁矿是内蒙古境内重要的铁矿之一,其矿源层赋存于温都尔庙群哈尔哈达组绢云母石英片岩型岩段中。
5) 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。
6) 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。
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