1) W-Au deposit
钨金矿
1.
The W-Au deposit (occurrences), being quartz vein type, is mainly distributed in NWW fault where is in northern Qinling Group and Shahewan rock body as a centre, It is distinct that zonation of W,W-Mo, Cu, Pb and Zn polymetals as well as the spatial distribution of Au and Ag mineralization present from south to north.
杨斜地区石英脉型钨金矿床(点)主要分布在以沙河湾岩体为中心的北侧秦岭群内北北西向断裂中。
2) copper-gold-tungsten deposits
铜金钨矿
3) Tungstengold
钨-金矿
6) Au-Sb-W deposit
金-锑-钨矿床
1.
REE geochemical evidence for the genesis of the Woxi Au-Sb-W deposit, Hunan Province;
湖南沃溪金-锑-钨矿床成因的稀土元素地球化学证据
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