Fe–Mg diffusion in olivine II: point defect chemistry, change of diffusion mechanisms and a model for calculation of diffusion coefficients in natural olivine-Reference-Cited by-同舟云学术

Fe–Mg diffusion in olivine II: point defect chemistry, change of diffusion mechanisms and a model for calculation of diffusion coefficients in natural olivine

Published:2007-05-23 Issue:6 Volume:34 Page:409-430
ISSN:0342-1791
Container-title:Physics and Chemistry of Minerals
language:en
Short-container-title:Phys Chem Minerals

Author:

Dohmen Ralf,Chakraborty Sumit

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,General Materials Science

Link

http://link.springer.com/content/pdf/10.1007/s00269-007-0158-6.pdf

Reference30 articles.

1. Bai Q, Kohlstedt DL (1993) Effects of chemical environment on the solubility and incorporation mechanism for hydrogen in olivine. Phys Chem Miner 19:460–471

2. Barkmann T, Cemic L (1996) Impedance spectroscopy and defect chemistry of fayalite. Phys Chem Miner 23:186–192

3. Barrer RM, Bartholomew RF, Rees LVC (1963) Ion exchange in porous crystals Part II. The relationship between self- and exchange-diffusion coefficients. J Phys Chem Solids 24:309–317

4. Brodholt J (1997) Ab initio calculations on point defects in forsterite (Mg2SiO4) and implications for diffusion and creep. Am Miner 82:1049–1053

5. Chakraborty S (1997) Rates and mechanisms of Fe–Mg interdiffusion in olivine at 980 –1,300 °C. J Geophys Res 102(B6):12317–12331

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