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Melting and mixing states of the Earth’s mantle after the Moon-forming impact
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“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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Cites
Hydrodynamic and Hydromagnetic Stability
Chandrasekhar, S., & Gillis, J. (1962) · Physics Today · doi:10.1063/1.3058072 · Cited by 10,517
A low mass for Mars from Jupiter’s early gas-driven migration
Walsh, K. J., Morbidelli, A., Raymond, S. N., O'Brien, D. P., & Mandell, A. M. (2011) · Nature · doi:10.1038/nature10201 · Cited by 1,241
A crystallizing dense magma ocean at the base of the Earth’s mantle
Labrosse, S., Hernlund, J. W., & Coltice, N. (2007) · Nature · doi:10.1038/nature06355 · Cited by 875
Satellite-sized planetesimals and lunar origin
HARTMANN, W. K., & Davis, D. R. (1975) · Icarus · doi:10.1016/0019-1035(75)90070-6 · Cited by 840
Making the Moon from a Fast-Spinning Earth: A Giant Impact Followed by Resonant Despinning
Ćuk, M., & Stewart, S. T. (2012) · Science · doi:10.1126/science.1225542 · Cited by 680
Forming a Moon with an Earth-like composition via a giant impact
Canup, R. M. (2012) · Science · doi:10.1126/science.1226073 · Cited by 656
The origin of the Moon and the single-impact hypothesis III
Benz, W., Cameron, A. G. W., & Melosh, H. J. (1989) · Icarus · doi:10.1016/0019-1035(89)90129-2 · Cited by 645
Linked magma ocean solidification and atmospheric growth for Earth and Mars
Elkins-Tanton, L. T. (2008) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2008.03.062 · Cited by 589
Core formation and the oxidation state of the Earth
Wade, J., & Wood, B. J. (2005) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2005.05.017 · Cited by 578
Late formation and prolonged differentiation of the Moon inferred from W isotopes in lunar metals
Touboul, M., Kleine, T., Bourdon, B., Palme, H., & Wieler, R. (2007) · Nature · doi:10.1038/nature06428 · Cited by 466
Oxygen Isotopes and the Moon-Forming Giant Impact
Wiechert, U., Halliday, A. N., Lee, D., Snyder, G. A., Taylor, L. A., & Rumble, D., III (2001) · Science · doi:10.1126/science.1063037 · Cited by 459
Rubie, D. C., Jacobson, S. A., Morbidelli, A., O'Brien, D. P., Young, E., de Vries, J., Nimmo, F., Palme, H., & Frost, D. J. (2014) · Icarus · doi:10.1016/j.icarus.2014.10.015 · Cited by 448
Geochemistry of mantle–core differentiation at high pressure
Li, J., & Agee, C. B. (1996) · Nature · doi:10.1038/381686a0 · Cited by 425
Effect of variation in density on the stability of superposed streams of Fluid
Taylor, G. I. (1931) · Proceedings of the Royal Society of London Series A Containing Papers of a Mathematical and Physical Character · doi:10.1098/rspa.1931.0115 · Cited by 421
Magma ocean formation due to giant impacts
Tonks, W. B., & Melosh, H. J. (1993) · Journal of Geophysical Research Atmospheres · doi:10.1029/92je02726 · Cited by 415
Early differentiation and volatile accretion recorded in deep-mantle neon and xenon
Mukhopadhyay, S. (2012) · Nature · doi:10.1038/nature11141 · Cited by 414
Equilibration in the aftermath of the lunar-forming giant impact
Pahlevan, K., & Stevenson, D. J. (2007) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2007.07.055 · Cited by 381
Self-citationMechanisms of metal–silicate equilibration in the terrestrial magma ocean
Rubie, D. C., Melosh, H. J., Reid, J. E., Liebske, C., & Righter, K. (2003) · Earth and Planetary Science Letters · doi:10.1016/s0012-821x(02)01044-0 · Cited by 344
A hydrocode equation of state for SiO 2
Melosh, H. J. (2007) · Meteoritics and Planetary Science · doi:10.1111/j.1945-5100.2007.tb01009.x · Cited by 341
The origin of the moon and the single-impact hypothesis I
Benz, W., Slattery, W. L., & Cameron, A. G. W. (1986) · Icarus · doi:10.1016/0019-1035(86)90088-6 · Cited by 334
Fluid Dynamics Of Core Formation
Stevenson, D. J. (1990) · Oxford University Press eBooks · doi:10.1093/oso/9780195066197.003.0014 · Cited by 322
Self-citationStructure and Freezing of MgSiO 3 Liquid in Earth's Lower Mantle
Stixrude, L. P., & Karki, B. B. (2005) · Science · doi:10.1126/science.1116952 · Cited by 315
Spontaneous small‐scale melt segregation in partial melts undergoing deformation
Stevenson, D. J. (1989) · Geophysical Research Letters · doi:10.1029/gl016i009p01067 · Cited by 296
Self-citationThe tungsten isotopic composition of the Earth’s mantle before the terminal bombardment
Willbold, M., Elliott, T. R., & Moorbath, S. E. (2011) · Nature · doi:10.1038/nature10399 · Cited by 284
Fiquet, G., Dewaele, A., Andrault, D., Kunz, M., & LeBihan, T. (2000) · Geophysical Research Letters · doi:10.1029/1999gl008397 · Cited by 282
Fluid Dynamics of a Terrestrial Magma Ocean
Solomatov, V. S. (2000) · University of Arizona Press eBooks · doi:10.2307/j.ctv1v7zdrp.23 · Cited by 277
182 W Evidence for Long-Term Preservation of Early Mantle Differentiation Products
Touboul, M., Puchtel, I. S., & Walker, R. J. (2012) · Science · doi:10.1126/science.1216351 · Cited by 260
Highly siderophile elements in Earth’s mantle as a clock for the Moon-forming impact
Jacobson, S. A., Morbidelli, A., Raymond, S. N., O'Brien, D. P., Walsh, K. J., & Rubie, D. C. (2014) · Nature · doi:10.1038/nature13172 · Cited by 259
Thermodynamics of silicate liquids in the deep Earth
Stixrude, L. P., de Koker, N., Sun, N., Mookherjee, M., & Karki, B. B. (2009) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2008.12.006 · Cited by 257
Righter, K., DRAKE, M. J., & Yaxley, G. M. (1997) · Physics of The Earth and Planetary Interiors · doi:10.1016/s0031-9201(96)03235-9 · Cited by 252
The oxygen‐isotopic composition of Earth and Mars
Franchi, I. A., Wright, I. P., Sexton, A. S., & Pillinger, C. T. (1999) · Meteoritics and Planetary Science · doi:10.1111/j.1945-5100.1999.tb01371.x · Cited by 210
Identification of the giant impactor Theia in lunar rocks
Herwartz, D., Pack, A., Friedrichs, B., & Bischoff, A. (2014) · Science · doi:10.1126/science.1251117 · Cited by 200
Tackley, P. J. (2011) · Earth-Science Reviews · doi:10.1016/j.earscirev.2011.10.001 · Cited by 199
Silicon Isotope Evidence Against an Enstatite Chondrite Earth
Fitoussi, C., & Bourdon, B. (2012) · Science · doi:10.1126/science.1219509 · Cited by 189
Resonances in the Early Evolution of the Earth-Moon System
Touma, J., & Wisdom, J. (1998) · The Astronomical Journal · doi:10.1086/300312 · Cited by 188
A hit-and-run giant impact scenario
Reufer, A., MEIER, M. M. M., Benz, W., & WIELER, R. (2012) · Icarus · doi:10.1016/j.icarus.2012.07.021 · Cited by 187
The age of ferroan anorthosite 60025: oldest crust on a young Moon?
Carlson, R. W., & Lugmair, G. W. (1988) · Earth and Planetary Science Letters · doi:10.1016/0012-821x(88)90095-7 · Cited by 183
Early evolution of the Earth: Accretion, atmosphere formation, and thermal history
Abe, Y., & Matsui, T. (1986) · Journal of Geophysical Research Atmospheres · doi:10.1029/jb091ib13p0e291 · Cited by 177
Dahl, T. W., & Stevenson, D. J. (2010) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2010.03.038 · Cited by 167
Self-citationHf-W Isotopic Evidence for Rapid Accretion and Differentiation in the Early Solar System
Lee, D., & Halliday, A. N. (1996) · Science · doi:10.1126/science.274.5294.1876 · Cited by 164
Armytage, R. M. G., Georg, R. B., Williams, H. M., & Halliday, A. N. (2011) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2011.10.032 · Cited by 161
Geochemical arguments for an Earth-like Moon-forming impactor
Dauphas, N., Burkhardt, C., Warren, P. H., & Teng, F. (2014) · Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences · doi:10.1098/rsta.2013.0244 · Cited by 158
de Koker, N., & Stixrude, L. P. (2009) · Geophysical Journal International · doi:10.1111/j.1365-246x.2009.04142.x · Cited by 150
Lee, D., Halliday, A. N., Snyder, G. A., & Taylor, L. A. (1997) · Science · doi:10.1126/science.278.5340.1098 · Cited by 148
Melt distribution in mantle rocks deformed in shear
Zimmerman, M. E., Zhang, S., Kohlstedt, D. L., & Karato, S. (1999) · Geophysical Research Letters · doi:10.1029/1999gl900259 · Cited by 139
Formation of an interconnected network of iron melt at Earth’s lower mantle conditions
Shi, C. Y., Zhang, L., Yang, W., Liu, Y., Wang, J., Meng, Y., Andrews, J. C., & Mao, W. L. (2013) · Nature Geoscience · doi:10.1038/ngeo1956 · Cited by 122
Nakajima, M., & Stevenson, D. J. (2014) · Icarus · doi:10.1016/j.icarus.2014.01.008 · Cited by 99
Self-citationThe feeding zones of terrestrial planets and insights into Moon formation
Kaib, N. A., & Cowan, N. B. (2015) · Icarus · doi:10.1016/j.icarus.2015.01.013 · Cited by 98
Canup, R. M. (2008) · Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences · doi:10.1098/rsta.2008.0101 · Cited by 90
A primordial origin for the compositional similarity between the Earth and the Moon
Mastrobuono-Battisti, A., Perets, H. B., & Raymond, S. N. (2015) · Nature · doi:10.1038/nature14333 · Cited by 82
Early evolution of the Earth–Moon system with a fast-spinning Earth
Wisdom, J., & Tian, Z. (2015) · Icarus · doi:10.1016/j.icarus.2015.02.025 · Cited by 77
Chemical fractionation in the silicate vapor atmosphere of the Earth
Pahlevan, K., Stevenson, D. J., & Eiler, J. M. (2010) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2010.10.036 · Cited by 72
Self-citationLunar-forming impacts: processes and alternatives
Canup, R. M. (2014) · Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences · doi:10.1098/rsta.2013.0175 · Cited by 58
Direct shock wave loading of MgSiO3 perovskite to lower mantle conditions and its equation of state
Deng, L., Gong, Z., & Fei, Y. (2008) · Physics of The Earth and Planetary Interiors · doi:10.1016/j.pepi.2008.07.043 · Cited by 16
Asymmetric shock heating and the terrestrial magma ocean origin of the Moon
Karato, S. (2014) · Proceedings of the Japan Academy Series B · doi:10.2183/pjab.90.97 · Cited by 15
Brief follow-up on recent studies of Theia’s accretion
Kaib, N. A., & Cowan, N. B. (2015) · Icarus · doi:10.1016/j.icarus.2015.06.019 · Cited by 13
Moon Formation from Multiple Large Impacts
Citron, R., Aharonson, O., Perets, H. B., & Genda, H. (2014) · LPI · Cited by 6
Melting Due to Impacts on Growing Proto-Planets
de Vries, J., Nimmo, F., Melosh, H. J., Jacobson, S. A., Morbidelli, A., & Rubie, D. C. (2014) · LPI · Cited by 2
An High-Precistion Semi-Analytical on-Hugoniot EOS for Geologic Materials
Sugita, S., Kurosawa, K., Kadono, T., & Sano, T. (2012) · Lunar and Planetary Science Conference · Cited by 1
Flagged first, then by citations
3 of the 62 references couldn’t be matched to a known paper.
Research works printed but not linked: 1
- Cameron, 1976, The origin of the Moon, Lunar Planet. Sci., VII, 120
Cited by
Sorted by citations
Secular change and the onset of plate tectonics on Earth
Palin, R. M., Santosh, M., Cao, W., Li, S.-S., Hernández-Uribe, D., & Parsons, A. (2020) · Earth-Science Reviews · doi:10.1016/j.earscirev.2020.103172 · Cited by 355
“magma ocean (or crystal-rich mush) to a depth of ~150–300 km below the surface (Hofmeister, 1983; Ohtani, 1985; Elkins-Tanton, 2012); 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 ocea…”
BackgroundThe Origin of the Moon Within a Terrestrial Synestia
Lock, S. J., Stewart, S. T., Petaev, M. I., Leinhardt, Z. M., Mace, M., Jacobsen, S. B., & Ćuk, M. (2018) · Journal of Geophysical Research Planets · doi:10.1002/2017je005333 · Cited by 328
Evaporation of moderately volatile elements from silicate melts: experiments and theory
Sossi, P. A., Klemme, S., O'Neill, H. S. C., Berndt, J., & Moynier, F. (2019) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2019.06.021 · Cited by 169
A multiple-impact origin for the Moon
Rufu, R., Aharonson, O., & Perets, H. B. (2017) · Nature Geoscience · doi:10.1038/ngeo2866 · Cited by 144
Kleine, T., & Walker, R. J. (2017) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev-earth-063016-020037 · Cited by 132
Metadata
- 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
- green
- arxiv.org
- 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 › Earth and Planetary Sciences › Space and Planetary Science › Astro and Planetary Science
- Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › 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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