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Explaining the dependence of M‑site difusion in forsterite on silica activity: a density functional theory approach

文献类型:期刊论文

作者Joshua M. R. Muir; Michael Jollands; Feiwu Zhang; Andrew M. Walker
刊名Physics and Chemistry of Minerals
出版日期2020
页码1-16
DOI10.1007/s00269-020-01123-5
URL标识查看原文
语种英语
源URL[http://ir.gyig.ac.cn/handle/42920512-1/11429]  
专题地球化学研究所_矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
作者单位1.Institute of Earth Sciences, University of Lausanne,1015 Lausanne, Switzerland
2.Institute of Geochemistry, Chinese Academy of Sciences, 99 West Lincheng Road, Guiyang 550081, Guizhou, China
3.Lamont-Doherty Earth Observatory, 61 Rt 9W, Palisades,NY 10964, USA
4.School of Earth and Environment, University of Leeds,Leeds LS2 9JT, UK
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GB/T 7714
Joshua M. R. Muir,Michael Jollands,Feiwu Zhang,et al. Explaining the dependence of M‑site difusion in forsterite on silica activity: a density functional theory approach[J]. Physics and Chemistry of Minerals,2020:1-16.
APA Joshua M. R. Muir,Michael Jollands,Feiwu Zhang,&Andrew M. Walker.(2020).Explaining the dependence of M‑site difusion in forsterite on silica activity: a density functional theory approach.Physics and Chemistry of Minerals,1-16.
MLA Joshua M. R. Muir,et al."Explaining the dependence of M‑site difusion in forsterite on silica activity: a density functional theory approach".Physics and Chemistry of Minerals (2020):1-16.

入库方式: OAI收割

来源:地球化学研究所

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