Cited by 215Astro and Planetary ScienceHigh-pressure geophysics and materialsGeological and Geochemical Analysis

Melting and mixing states of the Earth’s mantle after the Moon-forming impact

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Nakajima, Miki, Stevenson, David J.·2015·Earth and Planetary Science Letters

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Crossref · 10.1016/j.epsl.2015.06.023

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  • Numerical simulations of a giant impact thought to have formed the Earth-Moon system suggest that over 50 vol% of the Earth's mantle could have melted, indicating a magma ocean to at least 600 km depth.

    “however, numerical simulations of a giant impact thought to have formed the Earth-Moon system suggests that over 50 vol% of the Earth's mantle could have melted, indicating a magma ocean to at least 600 km depth”

    From Secular change and the onset of plate tectonics on Earth (2020) · cites this paper as Nakajima and Stevenson, 2015

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Authors
Nakajima, M., & Stevenson, D. J.
Affiliations
California Institute of Technology (US)
Corresponding author
Nakajima, Miki
Venue
Earth and Planetary Science Letters
Publisher
Elsevier BV
Published
2015-10
Volume
427
Pages
286-295
ISSN
0012-821X (ISSN-L)
OpenAlex
W1963088560
Cited by
215
References
62
Citations by year
2026: 16 · 2025: 25 · 2024: 24 · 2023: 21 · 2022: 16 · 2021: 15 · 2020: 21 · 2019: 22 · 2018: 23 · 2017: 17 · 2016: 13 · 2015: 1
FWCI
10.24
Type
journal article
Language
en
Open access
Locations
  • Earth and Planetary Science Letters (publishedVersion)
  • arXiv (Cornell University) (submittedVersion)
  • CaltechAUTHORS (California Institute of Technology) (submittedVersion)
  • arXiv (Cornell University)
Funders
NASA (NNX14AP26H)
Topics
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astro and Planetary Science
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
Keywords
Moon formation, giant impacts, Earth's mantle, mantle mixing, mantle melting, proto-Earth, impactor size, mantle heterogeneity, Rankine-Hugoniot equations, entropy increase, equation of state, forsterite, smoothed particle hydrodynamics

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