An Overview of Fe-Mg Interdiffusion in Mantle Minerals

被引：9
|
作者：
Zhang, Baohua [1 ]
机构：
[1] Chinese Acad Sci, Inst Geochem, Key Lab High Temp & High Pressure Study Earths In, Guiyang 550081, Peoples R China
来源：
SURVEYS IN GEOPHYSICS | 2017年 / 38卷 / 04期
关键词：
High temperature and high pressure; Mantle mineral; Fe-Mg interdiffusion; Point defects; CATION DIFFUSION; ALUMINOSILICATE GARNETS; OLIVINE; TEMPERATURE; PRESSURE; RATES; COMPENSATION; WADSLEYITE; HYDROGEN; CRYSTAL;
D O I：
10.1007/s10712-017-9415-5
中图分类号：
P3 [地球物理学]; P59 [地球化学];
学科分类号：
0708 ; 070902 ;
摘要：
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.
引用
收藏
页码：727 / 755
页数：29
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