High‐Pressure Phase Stability and Thermoelastic Properties of Iron Carbonitrides and Nitrogen in the Deep Earth-Reference-Cited by-同舟云学术

High‐Pressure Phase Stability and Thermoelastic Properties of Iron Carbonitrides and Nitrogen in the Deep Earth

Published:2021-06 Issue:6 Volume:126 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J Geophys Res Solid Earth

Author:

Huang Shengxuan¹²³^ORCID,Wu Xiang³^ORCID,Zhu Feng²,Lai Xiaojing⁴^ORCID,Li Jie⁵,Neill Owen K.⁵^ORCID,Qin Shan¹^ORCID,Rapp Robert²,Zhang Dongzhou²⁶^ORCID,Dera Przemyslaw²^ORCID,Chariton Stella⁶,Prakapenka Vitali B.⁶^ORCID,Chen Bin²^ORCID

Affiliation:

1. Key Laboratory of Orogenic Belts and Crustal Evolution MOE, Peking University and School of Earth and Space Sciences Peking University Beijing China

2. Hawaiʻi Institute of Geophysics and Planetology University of Hawaiʻi at Mānoa Honolulu HI USA

3. State Key Laboratory of Geological Processes and Mineral Resources China University of Geosciences Wuhan China

4. Gemmological Institute China University of Geosciences Wuhan China

5. Department of Earth and Environmental Sciences University of Michigan Ann Arbor MI USA

6. Center for Advanced Radiation Sources University of Chicago Chicago IL USA

Funder

National Science Foundation

National Natural Science Foundation of China

Peking University

U.S. Department of Energy

Chinese Academy of Sciences

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/10.1029/2021JB021934

Reference69 articles.

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5. Internally-Consistent Thermodynamic Data for Minerals in the System Na2O-K2O-CaO-MgO-FeO-Fe2O3-Al2O3-SiO2-TiO2-H2O-CO2

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