摘要
利用扫描电镜 -能谱对四川冕宁稀土矿床早期萤石的单个流体 -熔融包裹体中的成分进行了分析 ,发现包裹体内流体相阳离子以 Na、Ca、K、Ba为主 ,阴离子以 SO4、F、Cl为主 ,有意义的是在包裹体中发现了 L a、Ce、Nd等稀土元素 ,其中矿化元素铈的含量最高。
Scanning electron microscopy combined with energy dispersive analysis has been used to detect the composition of single fluid melt inclusion in fluorite formed in early stage Mianning REE deposit of Sichuan, China, The energy dispersive spectra show that the cations are dominated by Na, Ca, K, Ba, and anions by SO 4, F, Cl. Significantly, high contents of LREEs, La, Ce, Nd have been observed in the fluid inclusion, of which the content of the ore forming element Ce is the highest. These results further prove that the Mianning REE deposit in Sichuan is a hydrothermal deposit genetically related to salt melt.
出处
《岩石学报》
SCIE
EI
CAS
CSCD
北大核心
2000年第4期711-714,共4页
Acta Petrologica Sinica
基金
国家自然科学基金委 (合同批准号 49873 0 12 )
国家攀登预选计划 (95 -预 -3 9-0 1-0 4)资助
关键词
扫描电镜-能谱
流体-熔融包裹体
稀土矿床
地质
Scanning electron microscopy energy dispersive spectromicroscopy, Fluid inclusion, REE deposit