Diffusion in minerals at high pressure:: a review

被引：54

作者：

Béjina, F ^{[1
]}

Jaoul, O ^{[1
]}

Liebermann, RC ^{[1
]}

机构：

[1] CNRS, UMR 5563, Lab Mecanismes Transfert Geol, F-31000 Toulouse, France

来源：

PHYSICS OF THE EARTH AND PLANETARY INTERIORS | 2003年 / 139卷 / 1-2期

关键词：

high pressure; atomic diffusion; activation volume; point defects;

D O I：

10.1016/S0031-9201(03)00140-7

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：

There has been extensive technological progress in the last decade in performing diffusion experiments on minerals in solid-media, high-pressure (HP) apparatus. A database is presented which includes all extant data at pressures above 1 GPa. Measurements of activation volumes for the diffusion of silicon and divalent cations are compared for (FexMg1-x)O, quartz, olivine and its HP polymorphs (wadsleyite and ringwoodite), garnets and magnesium silicate perovskite. (C) 2003 Elsevier B.V. All rights reserved.

引用

页码：3 / 20

页数：18

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