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稀有金属伟晶岩锆石的REE特征、Zr/Hf和Y/Ho比值对岩浆-热液演化过程的指示 | |
吕正航; 张辉; 唐勇 | |
2013 | |
Source Publication | 矿物学报
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Issue | S2Pages:235-235 |
Keyword | Ree Y/ho Zr/hf 流体相 成矿过程 过渡阶段 晶体相 科学研究价值 钠长石 矿物组合 |
Subject Area | 地球深部物质与流体作用地球化学 |
Indexed By | CSCD |
Language | 中文 |
Citation statistics | |
Document Type | 期刊论文 |
Identifier | http://ir.gyig.ac.cn/handle/352002/5486 |
Collection | 地球内部物质高温高压实验室_地球内部物质高温高压实验室_期刊论文 |
Recommended Citation GB/T 7714 | 吕正航,张辉,唐勇. 稀有金属伟晶岩锆石的REE特征、Zr/Hf和Y/Ho比值对岩浆-热液演化过程的指示[J]. 矿物学报,2013(S2):235-235. |
APA | 吕正航,张辉,&唐勇.(2013).稀有金属伟晶岩锆石的REE特征、Zr/Hf和Y/Ho比值对岩浆-热液演化过程的指示.矿物学报(S2),235-235. |
MLA | 吕正航,et al."稀有金属伟晶岩锆石的REE特征、Zr/Hf和Y/Ho比值对岩浆-热液演化过程的指示".矿物学报 .S2(2013):235-235. |
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