REE characteristics of the Fanshan alunite deposit in Zhejiang Province, China | |
He YL(何玉良); Zhang Q(张乾); Shao SX(邵树勋); Zhu XQ(朱笑青); Zhu CH(祝朝辉); Wang DP(王大鹏) | |
通讯作者 | 张乾 |
2006 | |
发表期刊 | Chinese Journal of Geochemistry |
卷号 | 25期号:4页码:365-372 |
合作性质 | 其它 |
摘要 | REE geochemistry data from the Fanshan alunite deposit indicated that its ore-forming materials came chiefly from the country rocks, with δCe〉0 for alunite ores. According to the differences in δEu, the alunite ores were divided into three types: weak negative Eu anomaly, weak positive Eu anomaly and remarkable positive Eu anomaly. The phenomena of Ce-enrichment in the ores indicated that the Fanshan alunite deposit was formed in an oxidizing environment. Variations in fO2 are corresponding to those in δEu: Eu anomaly varies from negative to positive with increasing fO2. And two other important factors may impact the occurrence of Eu anomalies: the contents of alkaline feldspar and the protolith structure in the mineralization period. |
关键词 | Ree Characteristics |
资助者 | This research project was financially supported jointly by the Key Research Project (No. KZCX3-SW-125) of CAS and the National Natural Science Foundation of China (No. 40172037). |
收录类别 | CSCD |
语种 | 英语 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.gyig.ac.cn/handle/352002/572 |
专题 | 矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文 矿床地球化学国家重点实验室 |
通讯作者 | Zhang Q(张乾) |
推荐引用方式 GB/T 7714 | He YL,Zhang Q,Shao SX,et al. REE characteristics of the Fanshan alunite deposit in Zhejiang Province, China[J]. Chinese Journal of Geochemistry,2006,25(4):365-372. |
APA | He YL,Zhang Q,Shao SX,Zhu XQ,Zhu CH,&Wang DP.(2006).REE characteristics of the Fanshan alunite deposit in Zhejiang Province, China.Chinese Journal of Geochemistry,25(4),365-372. |
MLA | He YL,et al."REE characteristics of the Fanshan alunite deposit in Zhejiang Province, China".Chinese Journal of Geochemistry 25.4(2006):365-372. |
条目包含的文件 | ||||||
文件名称/大小 | 文献类型 | 版本类型 | 开放类型 | 使用许可 | ||
REE characteristics (453KB) | 开放获取 | 使用许可 | 浏览 请求全文 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。
修改评论