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Lanthanide tetrads with implications for liquid immiscibility in an evolving magmatic-hydrothermal system: Evidence from rare earth elements in zircon from the No. 112 pegmatite, Kelumute, Chinese Alt | |
Zheng-Hang Lv![]() ![]() ![]() | |
2018 | |
Source Publication | Journal of Asian Earth Sciences
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Volume | 164Pages:9-22 |
DOI | 10.1016/j.jseaes.2018.05.031 |
URL | 查看原文 |
Indexed By | SCI |
Language | 英语 |
WOS ID | WOS:000442706000002 |
Citation statistics | |
Document Type | 期刊论文 |
Identifier | http://ir.gyig.ac.cn/handle/42920512-1/14048 |
Collection | 地球内部物质高温高压实验室 地球深部物质与流体作用地球化学研究室 |
Affiliation | Key Laboratory of High-temperature and High-pressure Study of the Earth’s Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China |
Recommended Citation GB/T 7714 | Zheng-Hang Lv,Hui Zhang,Yong Tang. Lanthanide tetrads with implications for liquid immiscibility in an evolving magmatic-hydrothermal system: Evidence from rare earth elements in zircon from the No. 112 pegmatite, Kelumute, Chinese Alt[J]. Journal of Asian Earth Sciences,2018,164:9-22. |
APA | Zheng-Hang Lv,Hui Zhang,&Yong Tang.(2018).Lanthanide tetrads with implications for liquid immiscibility in an evolving magmatic-hydrothermal system: Evidence from rare earth elements in zircon from the No. 112 pegmatite, Kelumute, Chinese Alt.Journal of Asian Earth Sciences,164,9-22. |
MLA | Zheng-Hang Lv,et al."Lanthanide tetrads with implications for liquid immiscibility in an evolving magmatic-hydrothermal system: Evidence from rare earth elements in zircon from the No. 112 pegmatite, Kelumute, Chinese Alt".Journal of Asian Earth Sciences 164(2018):9-22. |
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Lanthanide tetrads w(2322KB) | 期刊论文 | 作者接受稿 | 开放获取 | CC BY-NC-SA | View Application Full Text |
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