High‐spin Fe 2+ and Fe 3+ in single‐crystal aluminous bridgmanite in the lower mantle-Reference-Cited by-同舟云学术

High‐spin Fe 2+ and Fe 3+ in single‐crystal aluminous bridgmanite in the lower mantle

Published:2016-07-14 Issue:13 Volume:43 Page:6952-6959
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Lin Jung‐Fu¹²,Mao Zhu³⁴,Yang Jing¹,Liu Jin¹,Xiao Yuming⁵,Chow Paul⁵,Okuchi Takuo⁶

Affiliation:

1. Department of Geological Sciences, Jackson School of Geosciences University of Texas at Austin Austin Texas USA

2. Center for High Pressure Science and Technology Advanced Research (HPSTAR) Shanghai China

3. Laboratory of Seismology and Physics of Earth's Interior, School of Earth and Planetary Sciences University of Science and Technology of China Hefei China

4. National Geophysics Observatory Mengcheng China

5. HPCAT, Geophysical Laboratory Carnegie Institution of Washington Argonne Illinois USA

6. Institute for Planetary Materials Okayama University Misasa Japan

Funder

Geophysics and CSEDI Programs of the NSF

Visiting Professorship Program of the Okayama University

DOE-NNSA

DOE-BES

NSF

263 DOE-BES

JSPS KAKENHI

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016GL069836

Reference50 articles.

1. Iron Partitioning in Earth's Mantle: Toward a Deep Lower Mantle Discontinuity

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

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

4. Ab initio study of the composition dependence of the pressure-induced spin crossover in perovskite (Mg1−x,Fex)SiO3

5. Mössbauer modeling to interpret the spin state of iron in (Mg,Fe)SiO3perovskite

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