1) W-Sn deposit
钨锡矿
1.
Geological features and origin of the Baigan Lake W-Sn deposit in the Ruoqiang area, East Kunlun Mountains, China.;
东昆仑山若羌地区白干湖钨锡矿床地质特征及成因
2.
Geological characteristics and ore-controlling factors of Da'ao greisen-type W-Sn deposit in South Hunan Province;
湖南大坳地区云英岩蚀变体型钨锡矿床地质特征及控矿因素
3.
This researches shows that the carbonate strata,emplacement of granite magma and faults are the important controlling factors of forming the W-Sn deposit in the studied area.
锡田地区矽卡岩型钨锡矿产于锡田花岗岩体哑铃柄部位的内外接触带。
2) W-Sn orefield
钨锡矿田
1.
A genetic study of Xinlu-Shuiyanba W-Sn orefield, northeast Guangxi;
广西新路—水岩坝钨锡矿田的成因探讨
3) tin and tungsten deposit
锡、钨矿
4) tungsten-tin ore
钨锡矿石
1.
According to characteristics of mineral processing technology for greisen-type micronization tungsten-tin ore of low grade.
针对大坳微细粒低品位云英岩型钨锡矿石的工艺特性,分别采用螺旋溜槽重选、阶段磨矿阶段选别的筛分摇床重选试验,并结合浮选试验,进行选矿工艺对比,采用阶段磨矿、阶段选别筛分摇床重选可取得较好的选矿效果,综合回收率达80。
5) tungsten-tin deposit
钨锡矿床
1.
The Da'ao tungsten-tin deposit in the Jiuyi Mountains,southern Hunan,is closely related to the Jinjiling composite granite which has the characteristics of aluminous A-type granite.
湘南九嶷山大坳钨锡矿床与具有铝质A型花岗岩特征的金鸡岭复式花岗岩关系密切。
2.
This paper focuses on the study of 40Ar/39Ar chronology of muscovite from three deposits: Keshuling and Piaotang tungsten-tin-multiple metals deposits(sulphide quartz vein type),and Xian etang tungsten-tin deposit(quartz vein type) in the Chongyi-Dayu-Shangyou concentrated mineral area.
由此表明,在崇余犹矿集区内存在两个不同成矿时期,即以黑钨矿为主的多金属硫化物石英脉型矿床形成于中侏罗世,集中于160~150Ma之间,与南岭地区钨锡矿床的主成矿期是一致的;而以锡石为主的,并含有大量白钨矿的石英脉型矿床可形成于印支期。
6) W-Sn deposits
钨锡矿床
1.
Based on the study of the granites,geochemistry,ore-control structures and geological characteristics of the W-Sn deposits,the authors propose that this area .
通过对区内花岗岩地质、地球化学、控矿构造及主要钨锡矿床地质特征分析研究,提出锡田地区具有良好的找矿前景。
补充资料：蓝钨氢还原(见仲钨酸铵氢还原)
蓝钨氢还原(见仲钨酸铵氢还原)
hydrogen reduction of blue tung sten compound
Ianwu qing huanyuan蓝钨氮还原(hydrogen reduetion of bluetungsten compound)见仲钨酸按氮还原。
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