Experimental Constraints on Solid Nitride Phases in Rocky Mantles of Reduced Planets and Implications for Observable Atmosphere Compositions

Author:

Daviau Kierstin1234ORCID,Lee Kanani K. M.156ORCID

Affiliation:

1. Department of Earth and Planetary Sciences Yale University New Haven CT USA

2. Department of Earth and Planetary Sciences Harvard University Cambridge MA USA

3. Now at University of Waikato (Tauranga) Tauranga New Zealand

4. Now at Toi‐Ohomai Institute of Technology Tauranga New Zealand

5. Now at Lawrence Livermore National Laboratory Livermore CA USA

6. Now at Department of Earth and Planetary Science University of California, Berkeley Berkeley CA USA

Funder

National Nuclear Security Administration

Basic Energy Sciences

National Science Foundation

Argonne National Laboratory

Lawrence Livermore National Laboratory

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference65 articles.

1. Thermal evolution and chemical differentiation of the terrestrial magma ocean;Abe Y.;Geophysical Monograph Series,1993

2. High-pressure Raman spectroscopy of diamond anvils to 250GPa: Method for pressure determination in the multimegabar pressure range

3. Diamond at high pressures: Raman scattering of light, equation of state, and high pressure scale;Aleksandrov I.;Zhurnal Eksperimental'noi i Teoreticheskoi Fiziki,1987

4. Temperature profiles in the Earth

5. Thermal pressure in the laser-heated diamond-anvil cell: An X-ray diffraction study

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