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Trace element partitioning between amphibole and hydrous silicate glasses at 0.6–2.6 GPa
Bo Zhang;  Xianxu Hu;  Peng Li;  Qizhe Tang;  Wenge Zhou
2019
Source PublicationActa Geochim
Volume38Issue:3Pages:414–429
KeywordAmphibole Silicate Glass Trace Elements Partition Coefficients Lattice Strain Model
Indexed ByEI
Language英语
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/10208
Collection地球内部物质高温高压实验室
Affiliation1.Key Laboratory for High Temperature and High Pressure Study of the Earth’s Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China
2.University of Chinese Academy of Sciences, Beijing 100049, China
3.Guizhou University of Finance and Economics, Guiyang 550025, China
4.Guizhou Institute of Technology, Guiyang 550003, China
Recommended Citation
GB/T 7714
Bo Zhang;Xianxu Hu;Peng Li;Qizhe Tang;Wenge Zhou. Trace element partitioning between amphibole and hydrous silicate glasses at 0.6–2.6 GPa[J]. Acta Geochim,2019,38(3):414–429.
APA Bo Zhang;Xianxu Hu;Peng Li;Qizhe Tang;Wenge Zhou.(2019).Trace element partitioning between amphibole and hydrous silicate glasses at 0.6–2.6 GPa.Acta Geochim,38(3),414–429.
MLA Bo Zhang;Xianxu Hu;Peng Li;Qizhe Tang;Wenge Zhou."Trace element partitioning between amphibole and hydrous silicate glasses at 0.6–2.6 GPa".Acta Geochim 38.3(2019):414–429.
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