Collisional erosion of mantle silicate during accretion can set the elevated Fe/Mg ratio of Earth

Authors

S. Charnoz (ORCID: https://orcid.org/0000-0002-7442-491X)
Julien Siebert (ORCID: https://orcid.org/0000-0001-9972-6239)
H. Genda
Miki Nakajima (ORCID: https://orcid.org/0000-0001-5014-0448)
Ryuki Hyodo (ORCID: https://orcid.org/0000-0003-4590-0988)
Sean N. Raymond (ORCID: https://orcid.org/0000-0001-8974-0758)
Seth A. Jacobson (ORCID: https://orcid.org/0000-0002-4952-9007)
Laëtitia Allibert (ORCID: https://orcid.org/0000-0002-5255-0990)

Publication Details

Journal: Icarus
Published: 2024-12-04
DOI: https://doi.org/10.1016/j.icarus.2024.116385
Citations: 1
Primary Topic: Astro and Planetary Science
Type: article
Field-Weighted Citation Impact: 0.33

Funders

National Science Foundation
National Aeronautics and Space Administration
Alfred P. Sloan Foundation
Deutsche Forschungsgemeinschaft
Agence Nationale de la Recherche
Nuclear Safety and Security Commission
Institut Universitaire de France
Labex UnivEarthS

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article

Collisional erosion of mantle silicate during accretion can set the elevated Fe/Mg ratio of Earth

S. Charnoz, Julien Siebert, H. Genda, Miki Nakajima et al.

Dec 4, 2024

1 citations

Icarus

Astro and Planetary Science

0.33

article

Collisional erosion of mantle silicate during accretion can set the elevated Fe/Mg ratio of Earth

S. Charnoz, Julien Siebert, H. Genda, Miki Nakajima, Ryuki Hyodo, Sean N. Raymond, Seth A. Jacobson, Laëtitia Allibert

December 4, 2024article en

1 citations

Abstract

No abstract available for this paper.

IcarusVol. 429

National Science Foundation, National Aeronautics and Space Administration, Alfred P. Sloan Foundation, Deutsche Forschungsgemeinschaft, Agence Nationale de la Recherche, Nuclear Safety and Security Commission, Institut Universitaire de France, Labex UnivEarthS

Climate action

Openalex Percentile: Top 33%

Astro and Planetary Science

0.33

DOI Open Access PDF OpenAlex

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