Articles | Volume 33, issue 1
© Author(s) 2021. This work is distributed underthe Creative Commons Attribution 4.0 License.
Influence of water on the physical properties of olivine, wadsleyite, and ringwoodite
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8 citations as recorded by crossref.
- Controls on the distribution of hydrous defects in forsterite from a thermodynamic model J. Muir et al. 10.1007/s00269-022-01182-w
- Sound Velocities of Superhydrous Phase B up to 21 GPa and 900 K C. Xu et al. 10.1029/2022GL098674
- First-principles study of water incorporation in Fe-containing wadsleyite T. Das et al. 10.1016/j.pepi.2022.106940
- Modelling hydrogen mobility in forsterite as diffusion coupled to inter-site reaction M. Jollands et al. 10.1007/s00410-022-01954-1
- Electrical conductivity of melts: implications for conductivity anomalies in the Earth's mantle B. Zhang et al. 10.1093/nsr/nwab064
- Water Solubility in Fe‐Bearing Wadsleyite at Mantle Transition Zone Temperatures H. Fei & T. Katsura 10.1029/2021GL092836
- The effect of oxygen fugacity on ionic conductivity in olivine H. Fei & T. Katsura 10.1016/j.gsf.2021.101270
- Behavior of hydrogen defect and framework of Fe-bearing wadsleyite and ringwoodite at high temperature and high pressure Y. Jin et al. 10.2138/am-2022-8544
Latest update: 28 Sep 2023