1) fluorite concentrate
萤石精矿
1.
The dewatering feature of the fluorite concentrate in Shizhuyuan Mine has been studied.
研究了柿竹园萤石精矿的脱水特性。
3) fluorite deposits
萤石矿床
1.
Aiming to the geological characters of fluorite deposits in Shuangjiangkou of Hunan,integrating the geological backgrounds,the geological conditions,the cause of formation of deposits and the factors of controlling ores in this district,the prospecting marks offluorite deposits have been suggested and the prospecting foreground is good.
针对双江口萤石矿床地质特征,结合区域地质背景、矿床地质条件、矿床成因和控矿因素,初步提出了找矿标志,该区具有较好的找矿前景。
4) Fluorite
[英]['fluərait] [美]['fluə,raɪt]
萤石矿
1.
The metallogenic characteristics of Huangshayao fluorite ore field and its exploitation;
黄沙腰萤石矿田成矿特征及找矿方向
2.
Iuvestigation and Evaluation of Labour Health Conditions in a Fluorite Mine;
某萤石矿劳动卫生条件调查评价
3.
The researchs on the fluorite deposits of Wuyi basin in Zhejiang show that the ore forming matter of the deposits comes from the wall rocks, the medium is meteoric water, the thermal source originates from tectonic magmatic activities and the mineralization temperature is 130℃±.
对浙江武义盆地萤石矿的研究表明，其成矿物质来自围岩，介质为大气降水，热源来自构造－岩浆活动，成矿温度为１３０℃±。
5) fluorite ores
萤石矿
1.
The Sanming area is located at the adjoiner of the Northwestern Fujian mole track and the Southwestern Fujian geotectogene and abundant in fluorite ores.
三明地区位于闽西北隆起带与闽西南坳陷带接合部 ,萤石矿资源丰富 ,其成矿受常口—瀚仙—余朋北东向断裂构造带控制。
6) fluorite deposit
萤石矿床
1.
REE geochemistry of fluorite from Yixian fluorite deposit and its geological implications;
义县萤石矿床稀土元素地球化学特征及其指示意义
2.
This paper has applied the cell- recurrence method and fractal box- counting method to the statistical analysis of 6 2 9fluorite deposits or ore spots in three different areas of Zhejiang Province.
本文应用单元递归法和分形丛集分析方法对浙江 3个不同区域范围内 6 2 9个萤石矿床 (点 )的空间及储量数据进行统计分析 ,揭示了这些矿床在空间上遵循分形丛集分布 ,在 0 。
3.
Most fluorite deposits from Guangdong, Fujian and Jiangxi Provinces of South China occur in the endo-or exdo-contact zone of granite intrusions.
华南地区广东、福建、江西等省内的萤石矿床，多数处于花岗岩的内外接触带上。
补充资料：反萤石结构
分子式：
CAS号：
性质：是A2B型离子晶体，其结构中阴离子B(如O2-)呈立方密堆积，阳离子A(如Na+)填充在四面体空隙中。阴、阳离子的配位数分别为8和4。阴、阳离子的这种排列方法恰恰与萤石结构相反，故名为反萤石结构。属反萤石结构的化合物有氧化钠、氧化钾和这些金属的硫属化合物等。
CAS号：
性质：是A2B型离子晶体，其结构中阴离子B(如O2-)呈立方密堆积，阳离子A(如Na+)填充在四面体空隙中。阴、阳离子的配位数分别为8和4。阴、阳离子的这种排列方法恰恰与萤石结构相反，故名为反萤石结构。属反萤石结构的化合物有氧化钠、氧化钾和这些金属的硫属化合物等。
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