Stability and Solubility of the FeAlO 3 Component in Bridgmanite at Uppermost Lower Mantle Conditions-Reference-Cited by-同舟云学术

Stability and Solubility of the FeAlO 3 Component in Bridgmanite at Uppermost Lower Mantle Conditions

Published:2020-02 Issue:2 Volume:125 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Liu Zhaodong¹²^ORCID,McCammon Catherine¹^ORCID,Wang Biao¹,Dubrovinsky Leonid¹,Ishii Takayuki¹^ORCID,Bondar Dmitry¹,Nakajima Ayano³,Tange Yoshinori⁴^ORCID,Higo Yuji⁴^ORCID,Cui Tian²,Liu Bingbing²,Katsura Tomoo¹⁵^ORCID

Affiliation:

1. Bayerisches GeoinstitutUniversity of Bayreuth Bayreuth Germany

2. State Key Laboratory of Superhard MaterialsJilin University Changchun China

3. Department of Earth Sciences, Graduate School of ScienceTohoku University Sendai Japan

4. SPring‐8Japan Synchrotron Radiation Institute Hyogo Japan

5. Center for High Pressure Science and Technology Advanced Research Beijing China

Funder

Deutsche Forschungsgemeinschaft

Servicestelle für Mobilitätsprogramme des österreichischen Bundesministeriums für Bildung, Wissenschaft und Forschung, KulturKontakt Austria

Horizon 2020 Framework Programme

National Natural Science Foundation of China

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/10.1029/2019JB018447

Reference69 articles.

1. The role of Al-defects on the equation of state of Al–(Mg,Fe)SiO3 perovskite

2. Equation of state of lower mantle (Al,Fe)-MgSiO3 perovskite

3. Large oxygen excess in the primitive mantle could be the source of the Great Oxygenation Event

4. Electronic Transitions in Perovskite: Possible Nonconvecting Layers in the Lower Mantle

5. Effect of chemistry on the compressibility of silicate perovskite in the lower mantle

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