1) 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。
2) 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。
3) Fluorite-barite mineral deposit
萤石-重晶石矿床
4) Au(Ag) fluorite ore deposit
金(银)-萤石矿床
1.
Studies show that the Au(Ag) fluorite ore deposit, a new type of gold deposits, was formed in the late stage of Yanshan and has been hosted in the Wuyi fluorite ore field.
江武义金（银）－萤石矿床，属燕山晚—末期成矿作用的产物。
5) monomineral-fluorite deposit
单一萤石矿床
1.
The Aobaotu fluorite deposit is a monomineral-fluorite deposit occurring at the contact zone between the volcanics-volcanogene sedimentary rocks of Lower Permian Dashizhai Formation and the Middle Yanshanian granitoid.
敖包吐萤石矿床产出于下二叠统大石寨组火山—沉积岩与燕山中期花岗岩的接触带,为单一萤石矿床。
6) Obotu fluorite deposit
敖包吐萤石矿床
1.
Sr,Nd and Pb isotopic geochemistry of fluorite from Obotu fluorite deposit,Inner Mongolia;
内蒙古敖包吐萤石矿床的Sr、Nd、Pb同位素地球化学特征
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