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Lanthanide tetrads in normalized rare element patterns of zircon from the Koktokay No. 3 granitic pegmatite, Altay, NW China
Tang Yong; Zhang Hui
2015
发表期刊American Mineralogist
卷号100期号:11-12页码:2630-2636
摘要
Individual crystals of zircon, from the Koktokay No. 3 granitic pegmatite vein, are variably altered and consist of three types of domains distinguished on the basis of textures and compositions. The pristine domains possess normal chondrite-normalized rare earth element (REE) patterns. Domains affected by metamictization are enriched in U and Th. The presence of abundant fractures, dense pores, and the enrichments of non-formula elements imply that these metamict domains have been altered by a later hydrothermal fluid. Tetrads observed in these altered domains are likely to have been generated by this alteration event. 
关键词Zircon Ree Tetrads Alteration Pegmatite Altay
学科领域地球深部物质与流体作用地球化学
收录类别SCI
语种英语
文献类型期刊论文
条目标识符http://ir.gyig.ac.cn/handle/352002/5761
专题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
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GB/T 7714
Tang Yong,Zhang Hui. Lanthanide tetrads in normalized rare element patterns of zircon from the Koktokay No. 3 granitic pegmatite, Altay, NW China[J]. American Mineralogist,2015,100(11-12):2630-2636.
APA Tang Yong,&Zhang Hui.(2015).Lanthanide tetrads in normalized rare element patterns of zircon from the Koktokay No. 3 granitic pegmatite, Altay, NW China.American Mineralogist,100(11-12),2630-2636.
MLA Tang Yong,et al."Lanthanide tetrads in normalized rare element patterns of zircon from the Koktokay No. 3 granitic pegmatite, Altay, NW China".American Mineralogist 100.11-12(2015):2630-2636.
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