1) Antimony deposits:ore-forming material
独山锑矿床
2) 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。
3) 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。
5) Xujiashan antimony deposit
徐家山锑矿床
1.
Characteristics of fluid inclusions in Xujiashan antimony deposit of Hubei Province and its implications;
湖北徐家山锑矿床流体包裹体特征及其意义
2.
Abstract: The Xujiashan antimony deposit is located in Tongshan County,Hubei Province,and its orebodies occurred in marine carbonates of the Upper Sinian Doushantuo and Dengying formations.
徐家山锑矿床位于湖北省通山县境内,矿体赋存于上震旦统灯影组和陡山沱组地层中。
补充资料：独妇山
1.山名。在浙江绍兴县西北。
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