REE geochemistry of primitive ore fluids in Ailaoshan gold belt, Southwest China

	REE geochemistry of primitive ore fluids in Ailaoshan gold belt, Southwest China
	Bi Xianwu;Hu Ruizhong
	1998
发表期刊	Chinese Journal of Geochemistry
卷号	17 期号:1 页码:91–96
摘要	The REE patterns of primitive ore solutions in the Ailaoshan gold belt are characterized by significant enrichment of LREE, a weak negative anomaly of Eu and a rather strong negative anomaly of Ce. In conjunction with the tension crust in the region, the ore solutions are thought to be originated from a CQ₂-rich fluid as a result of mantle degassing.
关键词	Ailaoshan Gold Belt Ore-forming Fluid Ree Geochemistry
收录类别	EI
语种	英语
文献类型	期刊论文
条目标识符	http://ir.gyig.ac.cn/handle/42920512-1/9441
专题	矿床地球化学国家重点实验室
作者单位	Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, 55000
推荐引用方式 GB/T 7714	Bi Xianwu;Hu Ruizhong. REE geochemistry of primitive ore fluids in Ailaoshan gold belt, Southwest China[J]. Chinese Journal of Geochemistry,1998,17(1):91–96.
APA	Bi Xianwu;Hu Ruizhong.(1998).REE geochemistry of primitive ore fluids in Ailaoshan gold belt, Southwest China.Chinese Journal of Geochemistry,17(1),91–96.
MLA	Bi Xianwu;Hu Ruizhong."REE geochemistry of primitive ore fluids in Ailaoshan gold belt, Southwest China".Chinese Journal of Geochemistry 17.1(1998):91–96.