1) The Xikuangshan type antimony deposits
锡矿山式锑矿
2) 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) 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) Xikuangshan type antimony deposits
锡矿山式梯矿床
6) tin-lead-stadium-zinc ore
锡铅锑锌矿
补充资料:辉锑矿(锡矿山矿务局)
辉锑矿(锡矿山矿务局)
黝黔…辉锑矿(‘矿山矿务”
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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