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1)  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
2)  Xintinling scheelite deposit
新田岭白钨矿床
1.
The Xintinling scheelite deposit, located in the northern contact zone of the Qitinling pluton, is a large-size skarn deposit.
新田岭白钨矿床是湘南W-Sn多金属矿集区中的一个大型矽卡岩型矿床,产于骑田岭岩体北接触带。
3)  Baiganhu tungsten-tin deposit
白干湖钨锡矿床
1.
Relations between Bashenerxi granite,west Dongkunlun and Baiganhu tungsten-tin deposit;
东昆仑西段巴什尔希花岗岩与白干湖钨锡矿床的关系
4)  Yanglin ao scheelite deposit
杨林坳白钨矿床
1.
Yanglin ao scheelite deposit is located at superposed site between the SN-trending Leiyang-Linwu fracture and NE-trending Liuyang-Hengyang fracture,on the west limb of SN-trending Chuankou uplift between Hengyang diwa and Youxian diwa of the Jiangxi-Guili diwa system in southeast geodepressional region.
杨林坳白钨矿床位于东南地洼区赣桂地洼系衡阳地洼与攸县地洼之间的川口南北向隆起之西翼,耒临南北向构造与浏衡北东向构造叠加复合部位。
5)  Sanjiazi Scheelite deposit
三家子白钨矿矿床
6)  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
补充资料:白钨矿
白钨矿
scheelite
    钨酸盐矿物。成分为Ca[WO4]。含WO380.6%,与黑钨矿同为钨的最主要工业矿物。四方晶系,晶体为近于八面体的四方双锥;通常呈不规则粒状或致密块状集合体。无色或白色,一般多呈灰色、浅黄、浅紫或浅褐色。玻璃光泽到金刚光泽,断口呈油脂光泽。解理中等,断口参差状。莫氏硬度4.5 ~5,比重大,达6.1。在紫外线照射下发浅蓝色荧光。主要产于花岗岩与石灰岩的接触交代夕卡岩中。中国湖南瑶岗仙和朝鲜南部的山塘都是世界有名的夕卡岩型白钨矿床。
    
   

白钨矿矿石

白钨矿矿石

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