The Effect of Water on Fe‐Mg Interdiffusion Rates in Ringwoodite and Implications for the Electrical Conductivity in the Mantle Transition Zone-Reference-Cited by-同舟云学术

The Effect of Water on Fe‐Mg Interdiffusion Rates in Ringwoodite and Implications for the Electrical Conductivity in the Mantle Transition Zone

Published:2019-03 Issue:3 Volume:124 Page:2510-2524
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Zhang Baohua¹^ORCID,Yoshino Takashi²^ORCID,Zhao Chengcheng²^ORCID

Affiliation:

1. Key Laboratory for High‐Temperature and High‐Pressure Study of the Earth's Interior, Institute of GeochemistryChinese Academy of Sciences Guiyang China

2. Institute for Planetary MaterialsOkayama University Tottori Japan

Funder

National Natural Science Foundation of China

Natural Science Foundation of Guizhou Province

Chinese Academy of Sciences

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB016415

Reference68 articles.

1. Electrical conductivity imaging of the Philippine Sea upper mantle using seafloor magnetotelluric data

2. Incorporation of water in iron-free ringwoodite: A first-principles study

3. A computer simulation study of OH defects in Mg2SiO4 and Mg2GeO4 spinels

4. Hydrogen mobility in transition zone silicates

5. Rates and mechanisms of Fe-Mg interdiffusion in olivine at 980°-1300°C

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