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

doi:10.1007/s00269-020-01123-5

CORC > 地球化学研究所 > 中国科学院地球化学研究所 > 矿床地球化学国家重点实验室 > 期刊论文

	Explaining the dependence of M‑site difusion in forsterite on silica activity: a density functional theory approach
	Joshua M. R. Muir ; Michael Jollands ; Feiwu Zhang ; Andrew M. Walker
刊名	Physics and Chemistry of Minerals
	2020
页码	1-16
DOI	10.1007/s00269-020-01123-5
URL标识	查看原文
语种	英语
内容类型	期刊论文
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.School of Earth and Environment, University of Leeds,Leeds LS2 9JT, UK 2.Lamont-Doherty Earth Observatory, 61 Rt 9W, Palisades,NY 10964, USA 3.Institute of Earth Sciences, University of Lausanne,1015 Lausanne, Switzerland 4.Institute of Geochemistry, Chinese Academy of Sciences, 99 West Lincheng Road, Guiyang 550081, Guizhou, China
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.