1) tungsten deposit
钨矿床
1.
Studies on the genesis and metallogenic model of Yanglin'ao tungsten deposit,Hengnan,Hunan province;
湖南衡南杨林坳钨矿床成因与成矿模式研究
2.
Fluid inclusion research of the tungsten deposit in south Jiangxi——Taking tungsten deposit of Xihuashan in Jiangxi province as an example;
赣南钨矿流体包裹体研究——以江西西华山钨矿床为例
3.
Geological features and fluid inclusions of Shamai tungsten deposit, Inner Mongolia;
内蒙古沙麦钨矿床地质及流体包裹体研究
2) W deposit
钨矿床
1.
Geological characteristics and enriching rules of the Hongling quartz-vein type W deposit in Guangdong;
广东红岭石英脉型钨矿床地质特征及富集规律
2.
Research on the ore-controlling factors and ore-forming rules of the Yanglin ao W deposit in Chuankou,Hunan;
湖南川口杨林坳钨矿床控矿因素与成矿规律研究
3.
Study of physical and chemical properties of hydroxo complex and alloy hydride of tungsten,chemical composition of fluid inclusion from W deposits,chemical composition of W minerals and mineral association in combination with geological setting suggests that tungsten was migrated as hydroxo complex and alloy hydride.
通过对钨羰基络合物及钨合金氢化物的物理化学性质、钨矿床矿物流体包裹体的化学组成、钨矿物的化学成分、主要共生伴生矿物组合的研讨,结合钨成矿的地质背景和环境,认为钨羰基络合物及钨合金氢化物是钨的主要迁移形式。
3) scheelite deposit
白钨矿床
1.
Geological characteristics of the Yangjin'gou scheelite deposit of Jilin and its ore genesis;
吉林杨金沟白钨矿床地质特征及成因探讨
2.
Geologic features and genesis of the Yangjingou scheelite deposit,Hunchun,Jilin Province;
吉林珲春杨金沟白钨矿床地质特征及成因初探
3.
Geologic features and genetic mechanism of the Yangjingou scheelite deposit,Hunchun City,Jilin Province;
吉林省珲春市杨金沟白钨矿床地质特征及成因机制探讨
4) 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。
5) 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