Extending the Solidus for a Model Iron‐Rich Martian Mantle Composition to 25 GPa-Reference-Cited by-同舟云学术

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Extending the Solidus for a Model Iron‐Rich Martian Mantle Composition to 25 GPa

Published:2018-10 Issue:19 Volume:45 Page:10,211-10,220
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Duncan Megan S.¹²^ORCID,Schmerr Nicholas C.³^ORCID,Bertka Constance M.⁴^ORCID,Fei Yingwei¹^ORCID

Affiliation:

1. Geophysical LaboratoryCarnegie Institution of Washington Washington DC USA

2. Now at Department of Earth and Planetary SciencesUniversity of California Davis CA USA

3. Department of GeologyUniversity of Maryland College Park MD USA

4. Science and Society Resources Rockland MD USA

Funder

National Aeronautics and Space Administration

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL078182

Reference38 articles.

1. Experimental constraints on the origin of Martian meteorites and the composition of the Martian mantle

2. Thermometry of the magma ocean: Controls on the metal–silicate partitioning of gold

3. Mineralogy of the Martian interior up to core-mantle boundary pressures

4. Density profile of an SNC model Martian interior and the moment-of-inertia factor of Mars

5. Anhydrous partial melting of an iron-rich mantle I: subsolidus phase assemblages and partial melting phase relations at 10 to 30 kbar

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4. Volatile and Trace Element Storage in a Crystallizing Martian Magma Ocean;Journal of Geophysical Research: Planets;2024-08

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