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
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出版日期 | 2020 |
页码 | 1-16 |
DOI | 10.1007/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 |
推荐引用方式 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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