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八尺稀土矿凝灰岩和花岗岩风化壳的细粒矿物特征
周军明; 袁鹏; 张佰发; 刘冬; 樊文枭
Source Publication2018年全国矿物科学与工程学术会议论文摘要文集
2018-07-06
Conference Date2018-07-06
Conference Place中国四川绵阳
Country中国
Indexed By其他
Language中文
Keyword花岗岩风化壳 细粒矿物 稀土元素 风化淋积型稀土矿 粘土矿物 凝灰岩
Abstract风化淋积型稀土矿床(又称作离子吸附型稀土矿床),是我国重要的稀土矿床,在我国分布广泛。该类稀土矿床是由花岗岩、凝灰岩等母岩风化而形成。其中花岗岩风化淋积型稀土矿床分布最广泛,其矿床成因、成矿规律等方面的研究也较为深入;而对凝灰岩风化淋积型稀土矿床的研究较少。风化淋积型稀土矿床中,粘土矿物等细粒矿物(粒径<2μm)物相及结构特征对探究稀土元素的赋存、迁移、分馏和富集具有
Document Type会议论文
Identifierhttp://ir.gig.ac.cn/handle/344008/35575
Collection中国科学院矿物学与成矿学重点实验室_会议论文
Recommended Citation
GB/T 7714
周军明,袁鹏,张佰发,等. 八尺稀土矿凝灰岩和花岗岩风化壳的细粒矿物特征[C],2018.
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