GYIG OpenIR  > 地球内部物质高温高压实验室  > 期刊论文
Petrogenesis and magmatic–hydrothermal evolution time limitation of Kelumute No. 112 pegmatite in Altay, Northwestern China: Evidence from zircon UPb and Hf isotopes
Zheng-Hang Lv; Hui Zhang; Yong Tang; Shen-Jin Guan
2012
Source PublicationLithos
Volume154Issue:1Pages:374-391
Indexed BySCI
Language英语
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/4664
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
Zheng-Hang Lv,Hui Zhang,Yong Tang,等. Petrogenesis and magmatic–hydrothermal evolution time limitation of Kelumute No. 112 pegmatite in Altay, Northwestern China: Evidence from zircon UPb and Hf isotopes[J]. Lithos,2012,154(1):374-391.
APA Zheng-Hang Lv,Hui Zhang,Yong Tang,&Shen-Jin Guan.(2012).Petrogenesis and magmatic–hydrothermal evolution time limitation of Kelumute No. 112 pegmatite in Altay, Northwestern China: Evidence from zircon UPb and Hf isotopes.Lithos,154(1),374-391.
MLA Zheng-Hang Lv,et al."Petrogenesis and magmatic–hydrothermal evolution time limitation of Kelumute No. 112 pegmatite in Altay, Northwestern China: Evidence from zircon UPb and Hf isotopes".Lithos 154.1(2012):374-391.
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