Garnero, E. J., McNamara, A. Okay. & Shim, S. H. Continent-sized anomalous zones with low seismic pace on the base of Earth’s mantle. Nat. Geosci. 9, 481–489 (2016).Article
CAS
Google Student
Labrosse, S., Hernlund, J. W. & Coltice, N. A crystallizing dense magma ocean on the base of the Earth’s mantle. Nature 450, 866–869 (2007).Article
CAS
PubMed
Google Student
Canup, R. M. & Asphaug, E. Foundation of the Moon in an enormous impression close to the top of the Earth’s formation. Nature 412, 708–712 (2001).Article
CAS
PubMed
Google Student
Kokubo, E. & Ida, S. Orbital evolution of protoplanets embedded in a swarm of planetesimals. Icarus 114, 247–257 (1995).Article
Google Student
Cameron, A. G. W. & Ward, W. R. The foundation of the Moon. Abstr. Lunar Planet. Sci. Conf. 7, 120–122 (1976).
Google Student
Ringwood, A. E. Risky and siderophile component geochemistry of the Moon: a reappraisal. Earth Planet. Sci. Lett. 111, 537–555 (1992).Article
CAS
Google Student
Nie, N. X. & Dauphas, N. Vapor drainage within the protolunar disk because the reason for the depletion in risky parts of the Moon. Astrophys. J. 884, L48 (2019).Article
CAS
Google Student
Lee, C. T. A. et al. Upside-down differentiation and technology of a primordial decrease mantle. Nature 463, 930–933 (2010).Article
CAS
PubMed
Google Student
Christensen, U. R. & Hofmann, A. W. Segregation of subducted oceanic crust within the convecting mantle. J. Geophys. Res. 99, 19867–19884 (1994).Article
CAS
Google Student
Williams, C. D., Mukhopadhyay, S., Rudolph, M. L. & Romanowicz, B. Primitive helium is sourced from seismically sluggish areas within the lowermost mantle. Geochem. Geophys. Geosyst. 20, 4130–4145 (2019).Article
CAS
Google Student
Mukhopadhyay, S. Early differentiation and risky accretion recorded in deep-mantle neon and xenon. Nature 486, 101–104 (2012).Article
CAS
PubMed
Google Student
Desch, S. J. & Robinson, Okay. L. A unified fashion for hydrogen within the Earth and Moon: nobody expects the Theia contribution. Chemie der Erde 79, 125546 (2019).Article
Google Student
Pepin, R. O. & Porcelli, D. Foundation of noble gases within the terrestrial planets. Rev. Mineral. Geochem. 47, 191–246 (2002).Article
CAS
Google Student
Burke, Okay., Steinberger, B., Torsvik, T. H. & Smethurst, M. A. Plume technology zones on the margins of enormous low shear pace provinces at the core–mantle boundary. Earth Planet. Sci. Lett. 265, 49–60 (2008).Article
CAS
Google Student
Will, P., Busemann, H., Riebe, M. E. I. & Maden, C. Indigenous noble gases within the Moon’s inside. Sci. Adv. 8, 1–9 (2022).Article
Google Student
Stewart, S. et al. The surprise physics of huge affects: key necessities for the equations of state. AIP Conf. Proc. 2272, 080003 (2020).Article
Google Student
Kegerreis, J. A., Eke, V. R., Massey, R. J., Sandnes, T. D. & Teodoro, L. F. A. Quick foundation of the Moon as a post-impact satellite tv for pc. Astrophys. J. Lett. 937, L40 (2022).Article
Google Student
Deng, H. et al. Enhanced blending in Large Have an effect on simulations with a brand new Lagrangian approach. Astrophys. J. 870, 127 (2019).Article
CAS
Google Student
Deng, H. et al. Primordial Earth mantle heterogeneity brought about by means of the Moon-forming Large Have an effect on? Astrophys. J. 887, 211 (2019).Article
CAS
Google Student
Cottaar, S. & Lekic, V. Morphology of seismically sluggish lower-mantle buildings. Geophys. J. Int. 207, 1122–1136 (2016).Article
Google Student
Kegerreis, J. A. et al. Planetary massive affects: convergence of high-resolution simulations the usage of environment friendly round preliminary stipulations and SWIFT. Mon. No longer. R. Astron. Soc. 487, 5029–5040 (2019).Article
CAS
Google Student
Deguen, R., Landeau, M. & Olson, P. Turbulent steel–silicate blending, fragmentation, and equilibration in magma oceans. Earth Planet. Sci. Lett. 391, 274–287 (2014).Article
CAS
Google Student
Dauphas, N., Burkhardt, C., Warren, P. H. & Fang-Zhen, T. Geochemical arguments for an Earth-like Moon-forming impactor. Philos. Trans. R. Soc. A 372, 20130244 (2014).Article
Google Student
Pahlevan, Okay., Stevenson, D. J. & Eiler, J. M. Chemical fractionation within the silicate vapor surroundings of the Earth. Earth Planet. Sci. Lett. 301, 433–443 (2011).Article
CAS
Google Student
Meier, M. M. M., Reufer, A. & Wieler, R. At the foundation and composition of Theia: constraints from new fashions of the Large Have an effect on. Icarus 242, 316–328 (2014).Article
CAS
Google Student
Robinson, Okay. L. et al. Water in developed lunar rocks: proof for a couple of reservoirs. Geochim. Cosmochim. Acta 188, 244–260 (2016).Article
CAS
Google Student
Connolly, J. A. D. Computation of segment equilibria by means of linear programming: a device for geodynamic modeling and its utility to subduction zone decarbonation. Earth Planet. Sci. Lett. 236, 524–541 (2005).Article
CAS
Google Student
Connolly, J. A. D. The geodynamic equation of state: what and the way. Geochem. Geophys. Geosyst. 10, 1–19 (2009).Article
Google Student
Stixrude, L. & Lithgow-Bertelloni, C. Thermodynamics of mantle minerals – II. Segment equilibria. Geophys. J. Int. 184, 1180–1213 (2011).Article
CAS
Google Student
Nakajima, M. & Stevenson, D. J. Melting and combining states of the Earth’s mantle after the Moon-forming impression. Earth Planet. Sci. Lett. 427, 286–295 (2015).Article
CAS
Google Student
Gurnis, M. The consequences of chemical density variations on convective blending within the Earth’s mantle. J. Geophys. Res., Forged Earth 91, 11407–11419 (1986).Article
Google Student
Tackley, P. J. in The Core‐Mantle Boundary Area (eds Gurnis, M., Wysession, M. E., Knittle, E. & Buffet, B. A.) 231–253 (American Geophysical Union, 1998).Nakagawa, T., Tackley, P. J., Deschamps, F. & Connolly, J. A. D. The affect of MORB and harzburgite composition on thermo-chemical mantle convection in a three-D round shell with self-consistently calculated mineral physics. Earth Planet. Sci. Lett. 296, 403–412 (2010).Article
CAS
Google Student
Gu, T., Li, M., McCammon, C. & Lee, Okay. Okay. M. Redox-induced decrease mantle density distinction and impact on mantle construction and primitive oxygen. Nat. Geosci. 9, 723–727 (2016).Article
CAS
Google Student
Yuan, Q. & Li, M. Instability of the African huge low-shear-wave-velocity province because of its low intrinsic density. Nat. Geosci. 15, 334–339 (2022).Article
CAS
Google Student
McNamara, A. Okay. & Zhong, S. Thermochemical buildings underneath Africa and the Pacific Ocean. Nature 437, 1136–1139 (2005).Article
CAS
PubMed
Google Student
O’Neill, C., Marchi, S., Zhang, S. & Bottke, W. Have an effect on-driven subduction at the Hadean Earth. Nat. Geosci. 10, 793–797 (2017).Article
Google Student
Hernlund, J. W. & Houser, C. At the statistical distribution of seismic velocities in Earth’s deep mantle. Earth Planet. Sci. Lett. 265, 423–437 (2008).Article
CAS
Google Student
Lei, W. et al. International adjoint tomography – fashion GLAD-M25. Geophys. J. Int. 223, 1–21 (2020).Article
Google Student
Elkins-Tanton, L. T. Magma oceans within the interior Sun Machine. Annu. Rev. Earth Planet. Sci. 40, 113–139 (2012).Article
CAS
Google Student
Abe, Y. Thermal and chemical evolution of the terrestrial magma ocean. Phys. Earth Planet. Inter. 1, 27–39 (1997).Article
Google Student
Solomatov, V. S. in Treatise on Geophysics 1st edn, Vol. 9 (ed. Schubert, G.) 91–119 (Elsevier, 2007).Maurice, M. et al. Onset of solid-state mantle convection and combining all the way through magma ocean solidification. J. Geophys. Res., Planets 122, 577–598 (2017).Article
Google Student
Boukaré, C. E., Parmentier, E. M. & Parman, S. W. Timing of mantle overturn all the way through magma ocean solidification. Earth Planet. Sci. Lett. 491, 216–225 (2018).Article
Google Student
Labrosse, S., Morison, A., Deguen, R. & Alboussière, T. Rayleigh–Bénard convection in a creeping stable with melting and freezing at both or each its horizontal barriers. J. Fluid Mech. 846, 5–36 (2018).Article
MathSciNet
CAS
MATH
Google Student
Agrusta, R. et al. Mantle convection interacting with magma oceans. Geophys. J. Int. 220, 1878–1892 (2020).Article
CAS
Google Student
Morison, A., Labrosse, S., Deguen, R. & Alboussière, T. Timescale of overturn in a magma ocean cumulate. Earth Planet. Sci. Lett. 516, 25–36 (2019).Article
CAS
Google Student
Becker, T. W., Kellogg, J. B. & O’Connell, R. J. Thermal constraints at the survival of primitive blobs within the decrease mantle. Earth Planet. Sci. Lett. 171, 351–365 (1999).Article
CAS
Google Student
Lock, S. J., Bermingham, Okay. R., Parai, R. & Boyet, M. Geochemical constraints at the foundation of the Moon and preservation of historic terrestrial heterogeneities. Area Sci. Rev. 216, 1–46 (2020).Article
Google Student
Ballmer, M. D., Lourenço, D. L., Hirose, Okay., Caracas, R. & Nomura, R. Reconciling magma-ocean crystallization fashions with the present-day construction of the Earth’s mantle. Geochem. Geophys. Geosyst. 18, 2785–2806 (2017).Article
CAS
Google Student
Maas, C. & Hansen, U. Dynamics of a terrestrial magma ocean below planetary rotation: a learn about in round geometry. Earth Planet. Sci. Lett. 513, 81–94 (2019).Article
CAS
Google Student
Williams, C. D. & Mukhopadhyay, S. Seize of nebular gases all the way through Earth’s accretion is preserved in deep-mantle neon. Nature 565, 78–81 (2019).Article
CAS
PubMed
Google Student
Mundl-Petermeier, A. et al. Temporal evolution of primordial tungsten-182 and 3He/4He signatures within the Iceland mantle plume. Chem. Geol. 525, 245–259 (2019).Article
CAS
Google Student
Li, M., McNamara, A. Okay. & Garnero, E. J. Chemical complexity of hotspots brought about by means of biking oceanic crust via mantle reservoirs. Nat. Geosci. 7, 366–370 (2014).Article
CAS
Google Student
Mulyukova, E., Steinberger, B., Dabrowski, M. & Sobolev, S. V. Survival of LLSVPs for billions of years in a vigorously convecting mantle: replenishment and destruction of chemical anomaly. J. Geophys. Res., Forged Earth 120, 3824–3847 (2015).Article
Google Student
Jackson, M. G. et al. Historic helium and tungsten isotopic signatures preserved in mantle domain names least changed by means of crustal recycling. Proc. Natl Acad. Sci. USA 117, 30993–31001 (2020).Article
CAS
PubMed
PubMed Central
Google Student
Brown, J. M. & Shankland, T. J. Thermodynamic parameters within the Earth as made up our minds from seismic profiles. Geophys. J. R. Astron. Soc. 66, 579–596 (1981).Article
MATH
Google Student
Stacey, F. D. A thermal fashion of the earth. Phys. Earth Planet. Inter. 15, 341–348 (1977).Article
Google Student
Canup, R. M., Barr, A. C. & Crawford, D. A. Lunar-forming affects: high-resolution SPH and AMR-CTH simulations. Icarus 222, 200–219 (2013).Article
Google Student
Hosono, N., Saitoh, T. R., Makino, J., Genda, H. & Ida, S. The Large Have an effect on simulations with density impartial smoothed particle hydrodynamics. Icarus 271, 131–157 (2016).Article
Google Student
Reinhardt, C. & Stadel, J. Numerical sides of Large Have an effect on simulations. Mon. No longer. R. Astron. Soc. 467, 4252–4263 (2017).Article
Google Student
Ruiz-Bonilla, S. et al. Coping with density discontinuities in planetary SPH simulations. Mon. No longer. R. Astron. Soc. 512, 4660–4668 (2022).Article
CAS
Google Student
Hosono, N. & Karato, S. The affect of equation of state at the Large Have an effect on simulations. J. Geophys. Res., Planets 127, 1–18 (2022).Article
Google Student
Hosono, N. et al. Unconvergence of very-large-scale Large Have an effect on simulations. Publ. Astron. Soc. Jpn 69, 1–11 (2017).Article
Google Student
Meier, T., Reinhardt, C. & Stadel, J. G. The EOS/decision conspiracy: convergence in proto-planetary collision simulations. Mon. No longer. R. Astron. Soc. 1816, 1806–1816 (2021).Article
Google Student
Raskin, C. & Owen, J. M. Analyzing the accuracy of astrophysical disk simulations with a generalized hydrodynamical take a look at drawback. Astrophys. J. 831, 26 (2016).Article
Google Student
Gabriel, T. S. J. & Allen-Sutter, H. Dependencies of mantle surprise heating in pairwise accretion. Astrophys. J. Lett. 915, L32 (2021).Article
Google Student
Frontiere, N., Raskin, C. D. & Owen, J. M. CRKSPH – a conservative reproducing kernel smoothed particle hydrodynamics scheme. J. Comput. Phys. 332, 160–209 (2017).Article
MathSciNet
MATH
Google Student
Rosswog, S. Astrophysical easy particle hydrodynamics. New Astron. Rev. 53, 78–104 (2009).Article
CAS
Google Student
Schaller, M. et al. SWIFT: SPH with inter-dependent fine-grained tasking. In Astrophysics Supply Code Library, ascl-1805 (2018).Ruiz-Bonilla, S., Eke, V. R., Kegerreis, J. A., Massey, R. J. &Teodoro, L. F. A. The impact of pre-impact spin at the Moon-forming collision. Mon. No longer. R. Astron. Soc. 2870, 2861–2870 (2021).
Google Student
Canup, R. M. Forming a Moon with an Earth-like composition by means of an enormous impression. Science 338, 1052–1056 (2012).Article
CAS
PubMed
PubMed Central
Google Student
Hopkins, P. F. A brand new magnificence of correct, mesh-free hydrodynamic simulation strategies. Mon. No longer. R. Astron. Soc. 450, 53–110 (2015).Article
CAS
Google Student
Thompson, S. L. & Lauson, H. S. Enhancements within the Chart D Radiation—Hydrodynamic Code. III. Revised Analytic Equation of State. Sandia Document SC-RR-71 0174 (1972).Melosh, H. J. A hydrocode equation of state for SiO2. Meteorit. Planet. Sci. 42, 2079–2098 (2007).Article
CAS
Google Student
Fiquet, G. et al. Melting of peridotite to 140 gigapascals. Science 329, 1516–1518 (2010).Article
CAS
PubMed
Google Student
Andrault, D. et al. Solidus and liquidus profiles of chondritic mantle: implication for melting of the Earth throughout its historical past. Earth Planet. Sci. Lett. 304, 251–259 (2011).Article
CAS
Google Student
Abe, Y. in Evolution of the Earth and Planets (eds Takahashi, E., Jeanloz, R. & Rubie, D.) 41–54 (American Geophysical Union, 1993).Miyazaki, Y. & Korenaga, J. At the timescale of magma ocean solidification and its chemical penalties: 2. Compositional differentiation below crystal accumulation and matrix compaction. J. Geophys. Res., Forged Earth 124, 3399–3419 (2019).Article
CAS
Google Student
Nomura, R. et al. Spin crossover and iron-rich silicate soften within the Earth’s deep mantle. Nature 473, 199–202 (2011).Article
CAS
PubMed
Google Student
Andrault, D. et al. Forged–liquid iron partitioning in Earth’s deep mantle. Nature 487, 354–357 (2012).Article
CAS
PubMed
Google Student
Moresi, L. N. & Solomatov, V. S. Numerical investigation of 2D convection with extraordinarily huge viscosity permutations. Phys. Fluids 7, 2154–2162 (1995).Article
MATH
Google Student
Farrell, Okay. A. O. & Lowman, J. P. Emulating the thermal construction of round shell convection in plane-layer geometry mantle convection fashions. Phys. Earth Planet. Inter. 182, 73–84 (2010).Article
Google Student
Tackley, P. J. & King, S. D. Trying out the tracer ratio approach for modeling energetic compositional fields in mantle convection simulations. Geochem. Geophys. Geosyst. 4, 1–15 (2003).Article
Google Student
Schaller, M. et al. Swift: a contemporary highly-parallel gravity and smoothed particle hydrodynamics solver for astrophysical and cosmological packages. Preprint at (2023).Hirth, G. & Kohlstedt, D. L. Water within the oceanic higher mantle: implications for rheology, soften extraction and the evolution of the lithosphere. Earth Planet. Sci. Lett. 144, 93–108 (1996).Article
CAS
Google Student
Dziewonski, A. M. & Anderson, D. L. Initial reference Earth fashion. Phys. Earth Planet. Inter. 25, 297–356 (1981).Article
Google Student