Phase relations in the Fe-Fe 3 C-Fe 3 N system at 7.8 GPa and 1350 °C: Implications for carbon and nitrogen hosts in Fe 0 -saturated upper mantle-Reference-Cited by-同舟云学术

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Phase relations in the Fe-Fe 3 C-Fe 3 N system at 7.8 GPa and 1350 °C: Implications for carbon and nitrogen hosts in Fe 0 -saturated upper mantle

Published:2017-04 Issue: Volume:265 Page:43-53
ISSN:0031-9201
Container-title:Physics of the Earth and Planetary Interiors
language:en
Short-container-title:Physics of the Earth and Planetary Interiors

Author:

Sokol Alexander G.,Kruk Alexey N.,Seryotkin Yurii V.,Korablin Alexander A.,Palyanov Yury N.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

Reference65 articles.

1. Graphite and diamond formation via the interaction of iron carbide and Fe, Ni-sulphide under mantle P-T parameters;Bataleva;Dokl. Earth Sci.,2016

2. HPHT synthesis of diamond with high nitrogen content from an Fe3N-C system;Borzdov;Diam. Relat. Mater.,2002

3. Nitrogen solubility in a molten assemblage of an (Fe, Ni) alloy and a CI chondritic silicate up to 18GPa;Bouhifd;Geochim. Cosmochim. Acta,2010

4. The formation of diamond;Bulanova;J. Geochem. Explor.,1995

5. Diamond genesis, mantle fractionations and mantle nitrogen content: a study of 13C-N concentrations in diamonds;Cartigny;Earth Planet. Sci. Lett.,2001

Cited by 16 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. The Fe(Ni)–C–N-phase diagram at 10 GPa—implications for nitrogen and carbon storage in the deep mantle;Contributions to Mineralogy and Petrology;2023-12-16

2. From the lithosphere to the lower mantle: An aqueous-rich metal-bearing growth environment to form type IIb blue diamonds;Chemical Geology;2022-12

3. Thermodynamic description of high-pressure phase equilibria in the Fe–N system;Journal of Alloys and Compounds;2022-09

4. Ultralow Melting of Iron Nitrides and the Fe–N–C System at High Pressure;Journal of Geophysical Research: Solid Earth;2022-02

5. Phase relations in the Fe-Fe3C-Fe3N system at 7.8 GPa and 1150°C: implications for C and N hosts in metal-saturated mantle;High Pressure Research;2021-10-02

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