GYIG OpenIR  > 地球内部物质高温高压实验室
An Overview of Fe-Mg Interdiffusion in Mantle Minerals
Baohua Zhang
2017
Source PublicationSurveys in Geophysics
Volume38Issue:4Pages:727–755
Abstract

The rates of Fe-Mg interdiffusion in the Earth's materials are of fundamental importance to a wide range of geochemistry and geophysics problems. In order that the Earth Scientist may readily apply the available experimentally determined diffusion rates to such problems, a brief review of experimental data for Fe-Mg interdiffusion in mantle minerals is presented concerning new advances and some recent applications. Perspectives for the future are also suggested.

KeywordHigh Temperature And High Pressure mantle Mineral fe–mg Interdiffusion point Defects
Indexed BySCI
Language英语
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/8083
Collection地球内部物质高温高压实验室
AffiliationKey Laboratory for High-Temperature and High-Pressure Study of the Earth’s Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China
Recommended Citation
GB/T 7714
Baohua Zhang. An Overview of Fe-Mg Interdiffusion in Mantle Minerals[J]. Surveys in Geophysics,2017,38(4):727–755.
APA Baohua Zhang.(2017).An Overview of Fe-Mg Interdiffusion in Mantle Minerals.Surveys in Geophysics,38(4),727–755.
MLA Baohua Zhang."An Overview of Fe-Mg Interdiffusion in Mantle Minerals".Surveys in Geophysics 38.4(2017):727–755.
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