Thermal conductivity anomaly in spin-crossover ferropericlase under lower mantle conditions and implications for heat flow across the core-mantle boundary-Reference-Cited by-同舟云学术

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Thermal conductivity anomaly in spin-crossover ferropericlase under lower mantle conditions and implications for heat flow across the core-mantle boundary

Published:2018-12-01 Issue:12 Volume:103 Page:1953-1958
ISSN:0003-004X
Container-title:American Mineralogist
language:en
Short-container-title:

Author:

Wu Zhongqing¹²

Affiliation:

1. Laboratory of Seismology and Physics of Earth's Interior, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China

2. National Geophysical Observatory at Mengcheng, University of Science and Technology of China, Anhui, China

Publisher

Mineralogical Society of America

Subject

Geochemistry and Petrology,Geophysics

Link

https://pubs.geoscienceworld.org/msa/ammin/article-pdf/103/12/1953/4574826/am-2018-6690.pdf

Cited by 3 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Evolution of Chemical Bonding and Spin-Pairing Energy in Ferropericlase across Its Spin Transition;ACS Earth and Space Chemistry;2022-03-03

2. The Transport Properties of Quasi–One-Dimensional Ba3Co2O6(CO3)0.7;Frontiers in Physics;2021-12-24

3. Anomalous thermal properties and spin crossover of ferromagnesite (Mg,Fe) CO3;Physical Review B;2021-02-01

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