1) karst accumulative bauxite deposit
岩溶堆积型铝土矿
1.
Karst accumulative bauxite deposit is a new type of deposit,and its mining method is particular as well as the reasons for ore dillution and loss and the controlling method used.
岩溶堆积型铝土矿是一种新的矿床类型 ,开采方法独特 ,贫化、损失产生的原因及其控制方法有其自身的特点 ,在多年的实践中 ,初步总结了开采该类型矿床的贫化、损失控制方
2) Karst accumulated bauxite
岩溶堆积铝土矿
1.
Taking the Jiaomei orefied in Pingguo Karst Accumulated Bauxite Area as an example,this paper makes detailed analysis on the characteristics of accumulating sequence of the bauxite in this area, puts forward a standard accumulating sequence and ideal distributing regularities of the Karst accumulated bauxite,which deepens the knowledge to the Karst accumulated bauxite in Pingguo or even in Guixi.
以平果堆积铝土矿教美矿区为例,对矿区堆积铝土矿的堆积序列特征进行了详细探析,提出了岩溶堆积铝土矿的标准堆积序列和理想分布规律,深化了对平果乃至桂西岩溶堆积铝土矿的认识。
3) accumulation-type bauxite
堆积型铝土矿
1.
Minerageny of gibbsite in accumulation-type bauxite deposits in western Guangxi;
桂西堆积型铝土矿中三水铝石成因矿物学研究
2.
Determination of accumulation-type bauxite and project separation;
论堆积型铝土矿勘查类型及工程网度的确定
3.
The serving time of some accumulation-type bauxite mine's industry establishment in existence was shortened greatly because of the reserves' lessening,the increase of its production capability and the change of other economic condition.
某堆积型铝土矿由于储量负变、产能增加及其他经济条件变化,使现有工业设施服务年限大大缩短,在周边经济合理寻求接替资源延长其服务年限势在必要。
4) Accumulated bauxite
堆积型铝土矿
1.
Metallogenic mechanism of gibbsite from accumulated bauxite in western Guangxi province;
桂西堆积型铝土矿中三水铝石的成矿机理
2.
Geological characteristics and remote sensing forecasting of accumulated bauxite of Pingguo
平果堆积型铝土矿地质特征及遥感找矿预测
5) karst type bauxite
岩溶型铝土矿
1.
The material source of the Carboniferous karst type bauxite in North China mainly came from the underlying Late Cambrian—Middle Ordovician carbonate rock.
华北石炭纪岩溶型铝土矿的主要物质来源为下伏的晚寒武世—中奥陶世碳酸盐岩。
6) accumulation bauxite deposit
堆积铝土矿
1.
It was proved in the past few years that the accumulation bauxite deposits in Pingguo and other places in western Guangxi are large-scale paragenetie deposits of gibbsite and diaspore.
近年证实平果等地堆积铝土矿是三水铝石硬水铝石共生的大型矿床。
补充资料：铝土矿
| 铝土矿 bauxite 以含水氧化铝为主、成分可变的天然多矿物混合物。主要由极细的三水铝石、软水铝石、硬水铝石和数量不等的粘土矿物、赤铁矿、针铁矿、石英等混合而成。含Al2O3量约40％～75％，是提炼铝的最主要矿石；也用来制取Al2O3，可作为磨料以及耐火材料。常呈豆状产出，但也呈块状、多孔状、土状等，随成因不同而异。颜色随氧化铁含量的增加，可呈白、灰直至棕红色，有时不同色彩呈斑点状分布。硬度和比重均较小，并随矿物组成不同而变化。铝土矿是由其母岩在湿热气候条件下经红土化作用而形成。由火成岩或变质岩形成的一般属红土型矿床，以三水铝石为主；由石灰岩或白云岩形成的，则属钙红土型，通常含有相当数量的软水铝石。风化壳铝土矿经剥蚀搬运，可形成沉积铝土矿。铝土矿分布广泛，法国的博奥是著名的重要产地；主要出产国有苏里南、牙买加、圭亚那等；中国广西、贵州、河南、山东等省也有广泛分布。 |
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