1) Xikuangshan antimony deposit
锡矿山锑矿床
1.
CALCULATION OF MASS TRANSFER IN ALTERED ROCKS——A case study of the Xikuangshan antimony deposit;
蚀变岩中物质迁移的定量计算——以锡矿山锑矿床为例
2.
Strontium isotope geochemistry of the Xikuangshan antimony deposit, Central Hunan;
湘中锡矿山锑矿床的Sr同位素地球化学
3.
As opinions about the genesis of Xikuangshan antimony deposit vary, no unanimous conclusion can be drawn.
锡矿山锑矿床的成因众说纷纭，笔者通过对矿区和区域构造的研究，并结合矿床的地球化学特征，发现该矿床是在伸展体制（时代从白垩纪至老第三纪）下由地下热液循环而形成的低温热液矿床，矿区的主要断裂对该矿床的形成具极其重要的控制作用。
3) The Xikuangshan type antimony deposits
锡矿山式锑矿
4) Xikuangshan ore field
锡矿山锑矿田
1.
Based on the study of geology and geochemistry of the Xikuangshan ore field and the location of lamprophyre veins, it is suggested that the location of lamprophyre veins do not mean the eastern boundary of the Xikuangshan ore field.
在研究矿田及煌斑岩脉附近地区地质地球化学特征的基础上，认为煌斑岩脉不是锡矿山锑矿田的东
5) Chashan antimony deposit
茶山锑矿床
1.
in this paper,through research of deposit geology, ore-forming nuid, ore bearing properties of Devonian system and REE geochemistry, the writer has summarized that theore -forming fluid is of hot-brine features in Chashan antimony deposit; and none of the evidence of genesis of magmatic hydrothermal solution was discovered.
本文通过矿床地质、成矿流体、泥盆系合矿性和稀土元素地球化学研究，总结出茶山锑矿床成矿流体具有热卤水特征，并未获得岩浆热液成因的证据。
6) Antimony deposits:ore-forming material
独山锑矿床
补充资料：精锑产品(锡矿山矿务局)
精锑产品(锡矿山矿务局)
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