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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; Hui Zhang; Yong Tang
2018
Source PublicationJournal of Asian Earth Sciences
Volume164Pages:9-22
DOI10.1016/j.jseaes.2018.05.031
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Indexed BySCI
Language英语
WOS IDWOS:000442706000002
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Cited Times:9[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://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
AffiliationKey Laboratory of High-temperature and High-pressure Study of the Earth’s Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China
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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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