Structure of sideriteFeCO3to 56 GPa and hysteresis of its spin-pairing transition-Reference-Cited by-同舟云学术

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Structure of sideriteFeCO3to 56 GPa and hysteresis of its spin-pairing transition

Published:2010-08-23 Issue:6 Volume:82 Page:
ISSN:1098-0121
Container-title:Physical Review B
language:en
Short-container-title:Phys. Rev. B

Author:

Lavina Barbara,Dera Przemyslaw,Downs Robert T.,Yang Wenge,Sinogeikin Stanislav,Meng Yue,Shen Guoyin,Schiferl David

Publisher

American Physical Society (APS)

Subject

Condensed Matter Physics,Electronic, Optical and Magnetic Materials

Link

http://harvest.aps.org/v2/journals/articles/10.1103/PhysRevB.82.064110/fulltext

Reference31 articles.

1. Experimental evidence for carbonate stability in the Earth's lower mantle

2. Stability of magnesite and its high-pressure form in the lowermost mantle

3. Fate of carbonates within oceanic plates subducted to the lower mantle, and a possible mechanism of diamond formation

4. Mantle-wide sequestration of carbon in silicates and the structure of magnesite II

5. The structure of some crystals as indicated by their diffraction of X-rays

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1. Constraints on the spin-state transition of siderite from laboratory-based Raman spectroscopy and electrical conductivity under high temperature and high pressure;Geoscience Frontiers;2024-08

2. Anomalous vibrational properties and spin phase diagrams of (Mg,Fe)CO3 under extreme conditions;Physical Review B;2024-06-24

3. Electrical conductivity of siderite and the effect of the spin transition of iron;Physics and Chemistry of Minerals;2024-05-23

4. High-Pressure Behavior of Ferromagnesite (Mg0.81Fe0.19)CO3 by Synchrotron X-Ray Diffraction and Raman Spectroscopy up to 53 GPa;Journal of Earth Science;2024-04

5. Electrical conductivity of siderite and the effect of the spin transition of iron;2024-02-08

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