1) Baiyun'ebo-Mandula
![点击朗读](/dictall/images/read.gif)
白云鄂博-满都拉
2) Bayan Obo
![点击朗读](/dictall/images/read.gif)
白云鄂博
1.
Types and Genesis of Na-Rich Rocks in the Bayan Obo REE-Nb-Fe Deposit, Inner Mongolia,China;
白云鄂博REE-Nb-Fe矿床的富钠岩石类型析及成因分
2.
Discussion on Proterozoic K- and REE-rich sedimentary rocks in North China as ore source of Bayan Obo rare earth deposits;
关于华北元古宙富钾、富稀土沉积岩是白云鄂博大型稀土矿床矿源层的讨论
3.
Laser Raman spectroscopy of typical rare-earth fluoro-carbonate minerals in Bayan Obo REE-Fe-Nb deposit and identification of rare-earth daughter minerals hosted in fluid inclusions.;
白云鄂博REE-Fe-Nb矿床稀土氟碳酸盐矿物激光拉曼光谱特征及流体包裹体内稀土子矿物的鉴定
3) Baiyunebo
![点击朗读](/dictall/images/read.gif)
白云鄂博
1.
Discussion on the Resources Potential of Baiyunebo Iron Mine and the Future Work Direction;
论白云鄂博铁矿资源潜力与今后地质工作方向
2.
Necessity and Feasibility of Baiyunebo Rare Earth Deposit Prospecting;
![点击朗读](/dictall/images/read.gif)
白云鄂博稀土矿床探矿的必要性与可行性探讨
3.
Reformation of ore matching method in Baiyunebo Iron Mine;
![点击朗读](/dictall/images/read.gif)
计算机技术在白云鄂博铁矿配矿管理中的应用
4) Baiyunebo deposit
![点击朗读](/dictall/images/read.gif)
白云鄂博矿
1.
The recoverable reserve of niobium in main open pit and east open pit is 80% of total reserve in Baiyunebo deposit, and the niobium minerals are fine in dissemination size and complex in intergrowth.
分析白云鄂博矿床铌资源的矿物学特征以及开发利用途径。
5) Bayan Obo Group
![点击朗读](/dictall/images/read.gif)
白云鄂博群
1.
Trace Elements Geochemistry of the Black Rock Series from Bayan Obo Group and Their Geological Implications;
白云鄂博群黑色岩系微量元素地球化学特征及地质意义
2.
A discussion on forming time of the Bayan Obo Group and ore-forming time of the Bayan Obo giant REE-Nb-Fe deposit,Inner Mongolia;
论内蒙古白云鄂博群和白云鄂博超大型稀土-铌-铁矿床成矿的年代
3.
Of these rocks, carbonaceous slate in the Agulugou Formation and siliceous-carbonaceous slate in Zenglongchang Formation of the Zhaertaishan Group and phyllitic slate in the Bilute Formation of the Bayan Obo Group are the best horizons bearing Pt and.
内蒙古渣尔泰山群和白云鄂博群是一套陆源碎屑岩、泥页岩、碳酸盐岩,地层中Pt、Pd的含量与原岩中泥质、有机碳、有机质的含量有关。
6) Baiyunebo Group
![点击朗读](/dictall/images/read.gif)
白云鄂博群
1.
Features and Regional Correlationon TwoMain Unconformity Interfaces in Baiyunebo Group, Inner Mongolia;
白云鄂博群中两个重要不整合界面特征及区域对比
2.
The Study of Sequence Stratigraphy of Baiyunebo Group;
![点击朗读](/dictall/images/read.gif)
白云鄂博群多重地层划分初探
3.
Folding of the middle-upper Proterozoic Jianshan Formation of Baiyunebo Group is very complex in Huaguoshan area of southeast Baiyunebo, northern margin of North China Platform.
华北地块北缘中上元古界的白云鄂博群尖山组 ,在白云鄂博群东南花果山一带褶皱变形十分复杂 ,为了研究其褶皱形态、变形机制 ,在原 1∶ 5万填图的基础上选近 1 km2的范围进行1∶ 2 0 0 0大比例尺地质填图 ,以变质长石石英砂岩为标志层 ,确定了两期褶皱构造。
补充资料:白云鄂博
白云鄂博 位于中国包头市北 150千米处的乌兰察布草原,周围是乌兰察布盟达 尔罕茂明安 联合旗辖地 。 白云鄂博为蒙古语,意为富饶的神山。白云鄂博铁矿位于白云鄂博矿区(属包头市)西北部,矿区面积138平方千米,全区人口 2.27 万。白云鄂博铁矿于1925年由地质学家丁道衡发现。1934年,著名地质学家、岩石矿物学家何作霖研究发现了白云鄂博矿的两种稀土元素新矿物,取名为白云矿与鄂博矿。至此,白云鄂博矿为世人所瞩目。1955年成立白云鄂博办事处 ,1958年成立白云鄂博镇(旗县级),8月划归包头市管辖。 |
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