Abstract
The Moon forming giant impact marks the end of the main stage of Earth’s accretion and sets the stage for the subsequent evolution of our planet. The giant impact theory has been the accepted model of lunar origin for 40 years, but the parameters of the impact and the mechanisms that led to the formation of the Moon are still hotly debated. Here we review the principal geochemical observations that constrain the timing and parameters of the impact, the mechanisms of lunar formation, and the contemporaneous evolution of Earth. We discuss how chemical and isotopic studies on lunar, terrestrial and meteorite samples relate to physical models and how they can be used to differentiate between lunar origin models. In particular, we argue that the efficiency of mixing during the collision is a key test of giant impact models. A high degree of intra-impact mixing is required to explain the isotopic similarity between the Earth and Moon but, at the same time, the impact did not homogenize the whole terrestrial mantle, as isotopic signatures of pre-impact heterogeneity are preserved. We summarize the outlook for the field and highlight the key advances in both measurements and modeling needed to advance our understanding of lunar origin.
Similar content being viewed by others
Notes
The mutual escape velocity is the minimum velocity required to overcome gravity and separate two bodies that are initially touching. Alternatively, the mutual escape velocity is the impact velocity of two bodies drawn together by gravity from infinite distance given zero initial relative velocity.
For the case of the post-impact Earth, the Roche limit is at a distance of about \(2.9~R_{\mathrm{Earth}}\) from the center of the body, where \(R_{\mathrm{Earth}}\) is the radius of the present-day Earth.
HSEs are those elements that have a strong propensity to be in metals over silicates and so are overwhelmingly incorporated into Earth’s core during accretion. Typically, HSEs are defined as elements that have metal–silicate partition coefficients (D values, concentration ratio of an element in liquid metal to liquid silicate) >10,000.
References
C. Agnor, R.M. Canup, H.F. Levison, On the character and consequences of large impacts in the late stage of terrestrial planet formation. Icarus 142(1), 219–237 (1999). https://doi.org/10.1006/icar.1999.6201
Y.A. Akovali, Nuclear data sheets for A = 244. Nucl. Data Sheets 99(1), 197–273 (2003). https://doi.org/10.1006/ndsh.2003.0008
F. Albarède, E. Albalat, C.T.A. Lee, An intrinsic volatility scale relevant to the Earth and Moon and the status of water in the Moon. Meteorit. Planet. Sci. 50(4), 568–577 (2015). https://doi.org/10.1111/maps.12331
C.J. Allègre, T. Staudacher, P. Sarda, M. Kurz, Constraints on evolution of Earth’s mantle from rare gas systematics. Nature 303(5920), 762–766 (1983). https://doi.org/10.1038/303762a0
D. Antonangeli, G. Morard, N.C. Schmerr, T. Komabayashi, M. Krisch, G. Fiquet, Y. Fei, H.K. Mao, Toward a mineral physics reference model for the Moon’s core. Proc. Natl. Acad. Sci. USA 112(13), 3916–3919 (2015). https://doi.org/10.1073/pnas.1417490112
R. Armytage, R. Georg, H. Williams, A. Halliday, Silicon isotopes in lunar rocks: implications for the Moon’s formation and the early history of the Earth. Geochim. Cosmochim. Acta 77, 504–514 (2012). https://doi.org/10.1016/j.gca.2011.10.032
R.M. Armytage, A.P. Jephcoat, M.A. Bouhifd, D. Porcelli, Metal-silicate partitioning of iodine at high pressures and temperatures: implications for the Earth’s core and 129*Xe budgets. Earth Planet. Sci. Lett. 373, 140–149 (2013). https://doi.org/10.1016/j.epsl.2013.04.031
E. Asphaug, Impact origin of the Moon? Annu. Rev. Earth Planet. Sci. 42(1), 551–578 (2014). https://doi.org/10.1146/annurev-earth-050212-124057
M. Barboni, P. Boehnke, B. Keller, I.E. Kohl, B. Schoene, E.D. Young, K.D. McKeegan, Early formation of the Moon 4.51 billion years ago. Sci. Adv. 3(1), e1602,365 (2017). https://doi.org/10.1126/sciadv.1602365
J.J. Barnes, R. Tartèse, M. Anand, F.M. McCubbin, C.R. Neal, I.A. Franchi, Early degassing of lunar urKREEP by crust-breaching impact(s). Earth Planet. Sci. Lett. 447, 84–94 (2016). https://doi.org/10.1016/j.epsl.2016.04.036
J.J. Barnes, I.A. Franchi, F.M. McCubbin, M. Anand, Multiple reservoirs of volatiles in the Moon revealed by the isotopic composition of chlorine in lunar basalts. Geochim. Cosmochim. Acta 266, 144–162 (2019). https://doi.org/10.1016/j.gca.2018.12.032
A.C. Barr, On the origin of Earth’s Moon. J. Geophys. Res., Planets 121(9), 1573–1601 (2016). https://doi.org/10.1002/2016JE005098
H. Becker, M.F. Horan, R.J. Walker, S. Gao, J.P. Lorand, R.L. Rudnick, Highly siderophile element composition of the Earth’s primitive upper mantle: constraints from new data on peridotite massifs and xenoliths. Geochim. Cosmochim. Acta 70(17), 4528–4550 (2006). https://doi.org/10.1016/j.gca.2006.06.004
A. Bischoff, Acfer 217 - a new member of the Rumuruti chondrite group (R). Meteoritics 29(2), 264–274 (1994). https://doi.org/10.1111/j.1945-5100.1994.tb00680.x
A. Bischoff, H. Palme, R.N. Clayton, T.K. Mayeda, T. Grund, B. Spettel, T. Geiger, M. Endreß, W. Beckerling, K. Metzler, New carbonaceous and type 3 ordinary chondrites from the Sahara Desert. Meteoritics 26, 318 (1991)
A. Bischoff, H. Palme, R.D. Ash, R.N. Clayton, L. Schultz, U. Herpers, D. Stöffler, M.M. Grady, C.T. Pillinger, B. Spettel, H. Weber, T. Grund, M. Endreß, D. Weber, Paired Renazzo-type (CR) carbonaceous chondrites from the Sahara. Geochim. Cosmochim. Acta 57(7), 1587–1603 (1993). https://doi.org/10.1016/0016-7037(93)90014-N
A. Bischoff, D. Weber, R. Bartoschewitz, R.N. Clayton, T.K. Mayeda, L. Schultz, B. Spettel, H.W. Weber, A. Bischoff, D. Weber, R. Bartoschewitz, R.N. Clayton, T.K. Mayeda, L. Schultz, B. Spettel, H.W. Weber, Characterization of the Rumuruti chondrite regolith breccia Hughes 030 (R3-6) and implications for the occurrence of unequilibrated lithologies on the R-chondrite parent body. Meteorit. Planet. Sci. 33, A15 (1998)
P. Bonnand, I.J. Parkinson, M. Anand, Mass dependent fractionation of stable chromium isotopes in mare basalts: implications for the formation and the differentiation of the Moon. Geochim. Cosmochim. Acta 175, 208–221 (2016). https://doi.org/10.1016/j.gca.2015.11.041
L.E. Borg, J.N. Connelly, M. Boyet, R.W. Carlson, Chronological evidence that the Moon is either young or did not have a global magma ocean. Nature 477(7362), 70–73 (2011). https://doi.org/10.1038/nature10328
L.E. Borg, A.M. Gaffney, T.S. Kruijer, N.A. Marks, C.K. Sio, J. Wimpenny, Isotopic evidence for a young lunar magma ocean. Earth Planet. Sci. Lett. 523, 115,706 (2019). https://doi.org/10.1016/j.epsl.2019.07.008
J.W. Boyce, A.H. Treiman, Y. Guan, C. Ma, J.M. Eiler, J. Gross, J.P. Greenwood, E.M. Stolper, The chlorine isotope fingerprint of the lunar magma ocean. Sci. Adv. 1(8), e1500,380 (2015). https://doi.org/10.1126/sciadv.1500380
J.W. Boyce, S.A. Kanee, F.M. McCubbin, J.J. Barnes, H. Bricker, A.H. Treiman, Early loss, fractionation, and redistribution of chlorine in the Moon as revealed by the low-Ti lunar mare basalt suite. Earth Planet. Sci. Lett. 500, 205–214 (2018). https://doi.org/10.1016/j.epsl.2018.07.042
M. Boyet, R.W. Carlson, A highly depleted moon or a non-magma ocean origin for the lunar crust? Earth Planet. Sci. Lett. 262(3–4), 505–516 (2007). https://doi.org/10.1016/j.epsl.2007.08.009
M. Boyet, J. Blichert-Toft, M. Rosing, M. Storey, P. Télouk, F. Albarède, 142Nd evidence for early Earth differentiation. Earth Planet. Sci. Lett. 214(3–4), 427–442 (2003). https://doi.org/10.1016/S0012-821X(03)00423-0
M. Boyet, A. Bouvier, P. Frossard, T. Hammouda, M. Garçon, A. Gannoun, Enstatite chondrites EL3 as building blocks for the Earth: the debate over the 146Sm–142Nd systematics. Earth Planet. Sci. Lett. 488, 68–78 (2018). https://doi.org/10.1016/j.epsl.2018.02.004
A.D. Brandon, T.J. Lapen, V. Debaille, B.L. Beard, K. Rankenburg, C. Neal, Re-evaluating 142Nd/144Nd in lunar mare basalts with implications for the early evolution and bulk Sm/Nd of the Moon. Geochim. Cosmochim. Acta 73(20), 6421–6445 (2009). https://doi.org/10.1016/j.gca.2009.07.015
A.J. Brearley, E.R. Scott, K. Keil, R.N. Clayton, T.K. Mayeda, W.V. Boynton, D.H. Hill, Chemical, isotopic and mineralogical evidence for the origin of matrix in ordinary chondrites. Geochim. Cosmochim. Acta 53(8), 2081–2093 (1989). https://doi.org/10.1016/0016-7037(89)90326-8
J.C. Bridges, I.A. Franchi, M.M. Grady, A.S. Sexton, C.T. Pillinger, The \(\delta\)18O composition of Feldspar and other minerals in Lafayette. Meteorit. Planet. Sci. 32(4), A21–A22 (1997)
J.C. Bridges, I.A. Franchi, A.S. Sexton, C.T. Pillinger, Mineralogical controls on the oxygen isotopic compositions of UOCs. Geochim. Cosmochim. Acta 63(6), 945–951 (1999). https://doi.org/10.1016/S0016-7037(98)00317-2
P.C. Buchanan, M.E. Zolensky, A.M. Reid, Carbonaceous chondrite clasts in the howardites Bholghati and EET87513. Meteoritics 28(5), 659–682 (1993). https://doi.org/10.1111/j.1945-5100.1993.tb00637.x
C. Burkhardt, N. Dauphas, H. Tang, M. Fischer-Gödde, L. Qin, J.H. Chen, S.S. Rout, A. Pack, P.R. Heck, D.A. Papanastassiou, In search of the Earth-forming reservoir: mineralogical, chemical, and isotopic characterizations of the ungrouped achondrite NWA 5363/NWA 5400 and selected chondrites. Meteorit. Planet. Sci. 52(5), 807–826 (2017). https://doi.org/10.1111/maps.12834
A.G.W. Cameron, W.R. Ward, The origin of the Moon, in Lunar and Planetary Science Conference Abstracts, vol. 7 (1976), p. 120
R.M. Canup, Simulations of a late lunar-forming impact. Icarus 168(2), 433–456 (2004). https://doi.org/10.1016/j.icarus.2003.09.028
R.M. Canup, Lunar-forming collisions with pre-impact rotation. Icarus 196(2), 518–538 (2008). https://doi.org/10.1016/j.icarus.2008.03.011
R.M. Canup, Forming a Moon with an Earth-like composition via a giant impact. Science 338(6110), 1052–1055 (2012). https://doi.org/10.1126/science.1226073
R.M. Canup, E. Asphaug, Origin of the Moon in a giant impact near the end of the Earth’s formation. Nature 412(6848), 708–712 (2001). https://doi.org/10.1038/35089010
R.M. Canup, C. Visscher, J. Salmon, B. Fegley Jr., Lunar volatile depletion due to incomplete accretion within an impact-generated disk. Nat. Geosci. 8(12), 918–921 (2015). https://doi.org/10.1038/ngeo2574
R.W. Carlson, L.E. Borg, A.M. Gaffney, M. Boyet, Rb-Sr, Sm-Nd and Lu-Hf isotope systematics of the lunar Mg-suite: the age of the lunar crust and its relation to the time of Moon formation. Philos. Trans. R. Soc. A, Math. Phys. Eng. Sci. 372(2024), 20130,246 (2014). https://doi.org/10.1098/rsta.2013.0246
R.W. Carlson, M. Garçon, J. O’Neil, J. Reimink, H. Rizo, The nature of Earth’s first crust. Chem. Geol. 530, 119,321 (2019). https://doi.org/10.1016/j.chemgeo.2019.119321
G. Caro, B. Bourdon, J.L. Birck, S. Moorbath, 146Sm-142Nd evidence from Isua metamorphosed sediments for early differentiation of the Earth’s mantle. Nature 423(6938), 428–432 (2003). https://doi.org/10.1038/nature01668
G. Caro, P. Morino, S.J. Mojzsis, N.L. Cates, W. Bleeker, Sluggish Hadean geodynamics: evidence from coupled 146, 147Sm–142, 143Nd systematics in Eoarchean supracrustal rocks of the Inukjuak domain (Québec). Earth Planet. Sci. Lett. 457, 23–37 (2017). https://doi.org/10.1016/j.epsl.2016.09.051
P.J. Carter, S.J. Lock, S.T. Stewart, The energy budgets of giant impacts. J. Geophys. Res., Planets 125(1), e2019JE006042 (2020). https://doi.org/10.1029/2019JE006042
S. Charnoz, C. Michaut, Evolution of the protolunar disk: dynamics, cooling timescale and implantation of volatiles onto the Earth. Icarus 260, 440–463 (2015). https://doi.org/10.1016/j.icarus.2015.07.018
S. Charnoz, Y. Lee, P. Sossi, L. Allibert, J. Siebert, R. Hyodo, H. Genda, F. Moynier, Efficient early Moon devolatilisation just after its formation, through tidally assisted hydrodynamic escape, in Lunar and Planetary Science Conference Abstracts, vol. 50 (2019), p. 2395
H. Chen, P.S. Savage, F.Z. Teng, R.T. Helz, F. Moynier, Zinc isotope fractionation during magmatic differentiation and the isotopic composition of the bulk Earth. Earth Planet. Sci. Lett. 369–370, 34–42 (2013). https://doi.org/10.1016/J.EPSL.2013.02.037
C.L. Chou, Fractionation of siderophile elements in the Earth’s upper mantle, in Lunar and Planetary Science Conference Abstracts, vol. 9 (1978), pp. 219–230
R.I. Citron, H.B. Perets, O. Aharonson, The role of multiple giant impacts in the formation of the Earth–Moon system. Astrophys. J. 862(1), 5 (2018). https://doi.org/10.3847/1538-4357/aaca2d
R.N. Clayton, T.K. Mayeda, Multiple parent bodies of polymict brecciated meteorites. Geochim. Cosmochim. Acta 42(3), 325–327 (1978). https://doi.org/10.1016/0016-7037(78)90185-0
R.N. Clayton, T.K. Mayeda, Redox processes in chondrules and chondrites, in Lunar and Planetary Science Conference Abstracts, vol. 12 (1981), pp. 154–156
R.N. Clayton, T.K. Mayeda, The oxygen isotope record in Murchison and other carbonaceous chondrites. Earth Planet. Sci. Lett. 67(2), 151–161 (1984). https://doi.org/10.1016/0012-821X(84)90110-9
R.N. Clayton, T.K. Mayeda, Oxygen isotopes in Shergotty, in Lunar and Planetary Science Conference Abstracts, vol. 16 (1985), p. 11
R.N. Clayton, T.K. Mayeda, Oxygen isotopic composition of LEW 86010. Meteoritics 24, 259 (1989)
R.N. Clayton, T.K. Mayeda, Oxygen isotopic composition of Antarctic meteorites, in Workshop on Differences Between Antarctic and non-Antarctic Meteorites, vol. 90-01 (1990), pp. 30–31
R.N. Clayton, T.K. Mayeda, Oxygen isotope studies of achondrites. Geochim. Cosmochim. Acta 60(11), 1999–2017 (1996). https://doi.org/10.1016/0016-7037(96)00074-9
R.N. Clayton, N. Onuma, T.K. Mayeda, A classification of meteorites based on oxygen isotopes. Earth Planet. Sci. Lett. 30(1), 10–18 (1976). https://doi.org/10.1016/0012-821X(76)90003-0
R.N. Clayton, N. Onuma, L. Grossman, T.K. Mayeda, Distribution of the pre-solar component in Allende and other carbonaceous chondrites. Earth Planet. Sci. Lett. 34(2), 209–224 (1977). https://doi.org/10.1016/0012-821X(77)90005-X
R.N. Clayton, T.K. Mayeda, E.J. Olsen, M. Prinz, Oxygen isotope relationships in iron meteorites. Earth Planet. Sci. Lett. 65(2), 229–232 (1983). https://doi.org/10.1016/0012-821X(83)90161-9
R. Clayton, T. Mayeda, K. Yanai, Oxygen isotopic compositions of some Yamato meteorites. Mem. Natl. Inst. Polar Res., Spec. Issue 35, 267–271 (1984a)
R.N. Clayton, T.K. Mayeda, A.E. Rubin, Oxygen isotopic compositions of enstatite chondrites and aubrites. J. Geophys. Res. 89(S01), C245 (1984b). https://doi.org/10.1029/jb089is01p0c245
R.N. Clayton, T.K. Mayeda, J.N. Goswami, E.J. Olsen, Oxygen isotope studies of ordinary chondrites. Geochim. Cosmochim. Acta 55(8), 2317–2337 (1991). https://doi.org/10.1016/0016-7037(91)90107-G
R.N. Clayton, T.K. Mayeda, T. Hiroi, M. Zolensky, M.E. Lipschutz, Oxygen isotopes in laboratory-heated CI and CM chondrites, in Annual Meteoritical Society Meeting, vol. 60 (1997a), p. 5255
R.N. Clayton, T.K. Mayeda, H. Kojima, M.K. Weisberg, M. Prinz, Hydration and dehydration in carbonaceous chondrites, in Lunar and Planetary Science Conference Abstracts, vol. 28 (1997b), p. 239
J.N. Connelly, M. Bizzarro, A.N. Krot, Å. Nordlund, D. Wielandt, M.A. Ivanova, The absolute chronology and thermal processing of solids in the solar protoplanetary disk. Science 338(6107), 651–655 (2012). https://doi.org/10.1126/science.1226919
H.C. Connolly, J. Zipfel, L. Folco, C. Smith, R.H. Jones, G. Benedix, K. Righter, A. Yamaguchi, H.C. Aoudjehane, J.N. Grossman, The Meteoritical Bulletin, No. 91, 2007 March. Meteorit. Planet. Sci. 42(3), 413–466 (2007). https://doi.org/10.1111/j.1945-5100.2007.tb00242.x
M. Ćuk, S.T. Stewart, Making the Moon from a fast-spinning Earth: a giant impact followed by resonant despinning. Science 338(6110), 1047–1052 (2012). https://doi.org/10.1126/science.1225542
M. Ćuk, D.P. Hamilton, S.J. Lock, S.T. Stewart, Tidal evolution of the Moon from a high-obliquity, high-angular-momentum Earth. Nature 539, 402–406 (2016). https://doi.org/10.1038/nature19846
C.W. Dale, T.S. Kruijer, K.W. Burton, Highly siderophile element and 182W evidence for a partial late veneer in the source of 3.8 Ga rocks from Isua, Greenland. Earth Planet. Sci. Lett. 458, 394–404 (2017). https://doi.org/10.1016/j.epsl.2016.11.001
N. Dauphas, The isotopic nature of the Earth’s accreting material through time. Nature 541(7638), 521–524 (2017). https://doi.org/10.1038/nature20830
N. Dauphas, C. Burkhardt, P.H. Warren, T. Fang-Zhen, Geochemical arguments for an Earth-like Moon-forming impactor. Philos. Trans. R. Soc. A, Math. Phys. Eng. Sci. 372(2024), 20130,244 (2014). https://doi.org/10.1098/rsta.2013.0244
N. Dauphas, M. Meheut, M. Blanchard, H. Zeng, G. Galli, R.N. Canup, C. Visscher, N. Nie, Can lunar formation theories be tested with K isotopes? in Lunar and Planetary Science Conference Abstracts, vol. 49 (2018), p. 2481
J.M. Day, F. Moynier, C.K. Shearer, Late-stage magmatic outgassing from a volatile-depleted Moon. Proc. Natl. Acad. Sci. USA 114(36), 9547–9551 (2017). https://doi.org/10.1073/pnas.1708236114
H. Deng, C. Reinhardt, F. Benitez, L. Mayer, J. Stadel, A.C. Barr, Enhanced mixing in giant impact simulations with a new Lagrangian method. Astrophys. J. 870(2), 127 (2019). https://doi.org/10.3847/1538-4357/aaf399
S.J. Desch, G.J. Taylor, Isotopic mixing due to the interaction between the protolunar disk and the Earth’s atmosphere, in Lunar and Planetary Science Conference Abstracts, vol. 44 (2013), p. 2566
J.K. Dhaliwal, J.M. Day, F. Moynier, Volatile element loss during planetary magma ocean phases. Icarus 300, 249–260 (2018). https://doi.org/10.1016/J.ICARUS.2017.09.002
J.E. Dickinson, P.C. Hess, Zircon saturation in lunar basalts and granites. Earth Planet. Sci. Lett. 57(2), 336–344 (1982). https://doi.org/10.1016/0012-821X(82)90154-6
E. Dowty, M. Prinz, K. Keil, Ferroan anorthosite: a widespread and distinctive lunar rock type. Earth Planet. Sci. Lett. 24(1), 15–25 (1974). https://doi.org/10.1016/0012-821X(74)90003-X
M.J. Drake, H.E. Newsom, C.J. Capobianco, V, Cr, and Mn in the Earth, Moon, EPB, and SPB and the origin of the Moon: Experimental studies. Geochim. Cosmochim. Acta 53(8), 2101–2111 (1989). https://doi.org/10.1016/0016-7037(89)90328-1
K.F. Eckerman, R.J. Westfall, J.C. Ryman, M. Cristy, Nuclear decay data files of the dosimetry research group No. ORNL/TM-12350. Tech. rep. Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (1993). https://doi.org/10.2172/10116928
L.T. Elkins-Tanton, S. Burgess, Q.Z. Yin, The lunar magma ocean: reconciling the solidification process with lunar petrology and geochronology. Earth Planet. Sci. Lett. 304(3–4), 326–336 (2011). https://doi.org/10.1016/j.epsl.2011.02.004
C.N. Foley, M. Wadhwa, L.E. Borg, P.E. Janney, R. Hines, T.L. Grove, The early differentiation history of Mars from 182W-142Nd isotope systematics in the SNC meteorites. Geochim. Cosmochim. Acta 69(18), 4557–4571 (2005). https://doi.org/10.1016/j.gca.2005.05.009
I.A. Franchi, T. Akagi, C.T. Pillinger, Laser fluorination of meteorites - small sample analysis of \(\delta\)17O and \(\delta\)18O. Meteoritics 27, 222 (1992)
I.A. Franchi, I.P. Wright, A.S. Sexton, C.T. Pillinger, The oxygen-isotopic composition of Earth and Mars. Meteorit. Planet. Sci. 34(4), 657–661 (1999). https://doi.org/10.1111/j.1945-5100.1999.tb01371.x
A.M. Friedman, J. Milsted, D. Metta, D. Henderson, J. Lerner, A.L. Harkness, D.J. Rokop, Alpha decay half lives of 148Gd 150Gd, and 146Sm. Radiochim. Acta 5(4), 192–194 (1966). https://doi.org/10.1524/ract.1966.5.4.192
A.M. Gaffney, L.E. Borg, A young solidification age for the lunar magma ocean. Geochim. Cosmochim. Acta 140, 227–240 (2014). https://doi.org/10.1016/j.gca.2014.05.028
R.F. Garcia, J. Gagnepain-Beyneix, S. Chevrot, P. Lognonné, Very preliminary reference Moon model. Phys. Earth Planet. Inter. 188(1–2), 96–113 (2011). https://doi.org/10.1016/j.pepi.2011.06.015
J.L. Gooding, T.K. Mayeda, R.N. Clayton, T. Fukuoka, Oxygen isotopic heterogeneities, their petrological correlations, and implications for melt origins of chondrules in unequilibrated ordinary chondrites. Earth Planet. Sci. Lett. 65(2), 209–224 (1983). https://doi.org/10.1016/0012-821X(83)90159-0
C.A. Goodrich, K. Keil, J.L. Berkley, J. Laul, M. Smith, J.F. Wacker, R.N. Clayton, T.K. Mayeda, Roosevelt County 027: a low-shock Ureilite with interstitial silicates and high noble gas concentrations. Meteoritics 22(3), 191–218 (1987). https://doi.org/10.1111/j.1945-5100.1987.tb00619.x
C. Göpel, J. Birck, Mn/Cr systematics: a tool to discriminate the origin of primitive meteorites? in Goldschmidt Conference Abstracts (2010), p. A348
M. Grady, D. Aylmer, G. Kurat, T. Ntaflos, U. Ott, H. Palme, B. Spettel, Yamato-82042: an unusual carbonaceous chondrite with CM affinities. Mem. Natl. Inst. Polar Res., Spec. Issue 46(46), 162–178 (1987)
D.W. Graham, Noble gas isotope geochemistry of mid-ocean ridge and ocean island basalts: characterization of mantle source reservoirs. Rev. Mineral. Geochem. 47(1), 247–317 (2002). https://doi.org/10.2138/rmg.2002.47.8
M.L. Grange, R.T. Pidgeon, A.A. Nemchin, N.E. Timms, C. Meyer, Interpreting U-Pb data from primary and secondary features in lunar zircon. Geochim. Cosmochim. Acta 101, 112–132 (2013). https://doi.org/10.1016/j.gca.2012.10.013
R.C. Greenwood, J.A. Barrat, M.F. Miller, M. Anand, N. Dauphas, I.A. Franchi, P. Sillard, N.A. Starkey, Oxygen isotopic evidence for accretion of Earth’s water before a high-energy Moon-forming giant impact. Sci. Adv. 4(3), eaao5928 (2018). https://doi.org/10.1126/sciadv.aao5928
J. Gross, A.H. Treiman, C.N. Mercer, Lunar feldspathic meteorites: constraints on the geology of the lunar highlands, and the origin of the lunar crust. Earth Planet. Sci. Lett. 388, 318–328 (2014)
J.N. Grossman, The Meteoritical Bulletin, No. 83, 1999 July. Meteorit. Planet. Sci. 34(S4), A169–A186 (1999). https://doi.org/10.1111/j.1945-5100.1999.tb01762.x
J.N. Grossman, J. Zipfel, The Meteoritical Bulletin, No. 85, 2001 September. Meteorit. Planet. Sci. 36(S9), A293–A322 (2001). https://doi.org/10.1111/j.1945-5100.2001.tb01542.x
J.N. Grossman, R.N. Clayton, T.K. Mayeda, Oxygen isotopes in the matrix of the Semarkona (LL3.0) chondrite. Meteoritics 22, 395 (1987)
M. Guitreau, M. Boyet, J.L. Paquette, A. Gannoun, Z. Konc, M. Benbakkar, K. Suchorski, J.M. Hénot, Hadean protocrust reworking at the origin of the Archean Napier Complex (Antarctica). Geochem. Perspect. Lett. 12, 7–11 (2019). https://doi.org/10.7185/geochemlet.1927
J. Halbout, M. Javoy, F. Robert, Oxygen isotopes in type 3 ordinary chondrites, in Lunar and Planetary Science Conference Abstracts, vol. 15 (1984), pp. 339–340
J. Halbout, F. Robert, M. Javoy, Oxygen and hydrogen isotope relations in water and acid residues of carbonaceous chondrites. Geochim. Cosmochim. Acta 50(8), 1599–1609 (1986). https://doi.org/10.1016/0016-7037(86)90123-7
C.L. Harper, S.B. Jacobsen, Evidence from coupled 147Sm-143Nd and 146Sm-142Nd systematics for very early (4.5 Gyr) differentiation of the Earth’s mantle. Nature 360(6406), 728–732 (1992). https://doi.org/10.1038/360728a0
W.K. Hartmann, D.R. Davis, Satellite-sized planetesimals and lunar origin. Icarus 24(4), 504–515 (1975). https://doi.org/10.1016/0019-1035(75)90070-6
E.H. Hauri, A.E. Saal, M.J. Rutherford, J.A. Van Orman, Water in the Moon’s interior: truth and consequences. Earth Planet. Sci. Lett. 409, 252–264 (2015). https://doi.org/10.1016/j.epsl.2014.10.053
G.F. Herzog, F. Moynier, F. Albarède, A.A. Berezhnoy, Isotopic and elemental abundances of copper and zinc in lunar samples, Zagami, Pele’s hairs, and a terrestrial basalt. Geochim. Cosmochim. Acta 73(19), 5884–5904 (2009). https://doi.org/10.1016/j.gca.2009.05.067
M.F. Horan, R.W. Carlson, R.J. Walker, M. Jackson, M. Garçon, M. Norman, Tracking Hadean processes in modern basalts with 142-Neodymium. Earth Planet. Sci. Lett. 484, 184–191 (2018). https://doi.org/10.1016/j.epsl.2017.12.017
N. Hosono, Si. Karato, J. Makino, T.R. Saitoh, Terrestrial magma ocean origin of the Moon. Nat. Geosci. 12(6), 418–423 (2019). https://doi.org/10.1038/s41561-019-0354-2
M. Humayun, A model for osmium isotopic evolution of metallic solids at the core-mantle boundary. Geochem. Geophys. Geosyst. Q03, 007 (2011). https://doi.org/10.1029/2010GC003281
S. Ida, R.M. Canup, G.R. Stewart, Lunar accretion from an impact-generated disk. Nature 389(6649), 353–357 (1997). https://doi.org/10.1038/38669
A.V. Ivanov, A.A. Ulyanov, V.I. Ustinov, Y.A. Shukolyukov, The Kaidun meteorite: oxygen isotopic composition, in Lunar and Planetary Science Conference Abstracts, vol. 18 (1987), p. 453
I. Jabeen, M. Kusakabe, K. Nagao, T. Nakamura, Oxygen isotope study of Tsukuba chondrite, some HED meteorites and Allende chondrules. Antarct. Meteor. Res. 11, 122–135 (1998)
A. Jackel, A. Bischoff, R.N. Clayton, T.K. Mayeda, Dar AL Gani 013—a new Saharan Rumuruti-chondrite (R3-6) with highly unequilibrated (type 3) fragments, in Lunar and Planetary Science Conference Abstracts, vol. 27 (1996), p. 595
C.R. Jackson, N.R. Bennett, Z. Du, E. Cottrell, Y. Fei, Early episodes of high-pressure core formation preserved in plume mantle. Nature 553(7689), 491–495 (2018). https://doi.org/10.1038/nature25446
S.B. Jacobsen, M.I. Petaev, S. Huang, D.D. Sasselov, An isotopically homogeneous region of the inner terrestrial planet region (Mercury to Earth): evidence from E chondrites and implications for giant Moon-forming impact scenarios, in Lunar and Planetary Science Conference Abstracts, vol. 44 (2013), p. 2344
S.A. Jacobson, A. Morbidelli, S.N. Raymond, D.P. O’Brien, K.J. Walsh, D.C. Rubie, Highly siderophile elements in Earth’s mantle as a clock for the Moon-forming impact. Nature 508(1), 84–87 (2014). https://doi.org/10.1038/nature13172
Z. Jing, Y. Wang, Y. Kono, T. Yu, T. Sakamaki, C. Park, M.L. Rivers, S.R. Sutton, G. Shen, Sound velocity of Fe-S liquids at high pressure: implications for the Moon’s molten outer core. Earth Planet. Sci. Lett. 396, 78–87 (2014). https://doi.org/10.1016/j.epsl.2014.04.015
T.D. Jones, D.R. Davies, P.A. Sossi, Tungsten isotopes in mantle plumes: heads it’s positive, tails it’s negative. Earth Planet. Sci. Lett. 506, 255–267 (2019). https://doi.org/10.1016/j.epsl.2018.11.008
G.W. Kallemeyn, A.E. Rubin, J.T. Wasson, The compositional classification of chondrites: VII. The R chondrite group. Geochim. Cosmochim. Acta 60(12), 2243–2256 (1996). https://doi.org/10.1016/0016-7037(96)88430-4
Y. Kaspi, G.R. Flierl, A.P. Showman, The deep wind structure of the giant planets: results from an anelastic general circulation model. Icarus 202(2), 525–542 (2009). https://doi.org/10.1016/j.icarus.2009.03.026
C. Kato, F. Moynier, Gallium isotopic evidence for extensive volatile loss from the Moon during its formation. Sci. Adv. 3(7), e1700,571 (2017). https://doi.org/10.1126/sciadv.1700571
C. Kato, F. Moynier, M.C. Valdes, J.K. Dhaliwal, J.M.D. Day, Extensive volatile loss during formation and differentiation of the Moon. Nat. Commun. 6(1), 7617 (2015). https://doi.org/10.1038/ncomms8617
L.P. Keller, K.L. Thomas, R.N. Clayton, T.K. Mayeda, J.M. DeHart, D.S. McKay, Aqueous alteration of the Bali CV3 chondrite: evidence from mineralogy, mineral chemistry, and oxygen isotopic compositions. Geochim. Cosmochim. Acta 58(24), 5589–5598 (1994). https://doi.org/10.1016/0016-7037(94)90252-6
K. Kimura, R.S. Lewis, E. Anders, Distribution of gold and rhenium between nickel-iron and silicate melts: implications for the abundance of siderophile elements on the Earth and Moon. Geochim. Cosmochim. Acta 38(5), 683–701 (1974). https://doi.org/10.1016/0016-7037(74)90144-6
T. Kleine, R.J. Walker, Tungsten isotopes in planets. Annu. Rev. Earth Planet. Sci. 45(1), 389–417 (2017). https://doi.org/10.1146/annurev-earth-063016-020037
T. Kleine, M. Touboul, B. Bourdon, F. Nimmo, K. Mezger, H. Palme, S.B. Jacobsen, Q.Z. Yin, A.N. Halliday, Hf–W chronology of the accretion and early evolution of asteroids and terrestrial planets. Geochim. Cosmochim. Acta 73(17), 5150–5188 (2009). https://doi.org/10.1016/j.gca.2008.11.047
E. Kokubo, H. Genda, Formation of terrestrial planets from protoplanets under a realistic accretion condition. Astrophys. J. 714(1), L21–L25 (2010). https://doi.org/10.1088/2041-8205/714/1/L21
E. Kokubo, S. Ida, J. Makino, Evolution of a circumterrestrial disk and formation of a single moon. Icarus 148(2), 419–436 (2000). https://doi.org/10.1006/icar.2000.6496
T.S. Kruijer, T. Kleine, Tungsten isotopes and the origin of the Moon. Earth Planet. Sci. Lett. 475, 15–24 (2017). https://doi.org/10.1016/j.epsl.2017.07.021
T.S. Kruijer, T. Kleine, No 182W excess in the Ontong Java Plateau source. Chem. Geol. 485, 24–31 (2018). https://doi.org/10.1016/j.chemgeo.2018.03.024
T.S. Kruijer, T. Kleine, M. Fischer-Gödde, P. Sprung, Lunar tungsten isotopic evidence for the late veneer. Nature 520, 534–537 (2015). https://doi.org/10.1038/nature14360
M.D. Kurz, W.J. Jenkins, S.R. Hart, Helium isotopic systematics of oceanic islands and mantle heterogeneity. Nature 297(5861), 43–47 (1982). https://doi.org/10.1038/297043a0
K.K. Larsen, A. Trinquier, C. Paton, M. Schiller, D. Wielandt, M.A. Ivanova, J.N. Connelly, Å. Nordlund, A.N. Krot, M. Bizzarro, Evidence for magnesium isotope heterogeneity in the solar protoplanetary disk. Astrophys. J. Lett. 735(2), L37 (2011). https://doi.org/10.1088/2041-8205/735/2/L37
C. Li, D. Liu, B. Liu, X. Ren, J. Liu, Z. He, W. Zuo, X. Zeng, R. Xu, X. Tan, X. Zhang, W. Chen, R. Shu, W. Wen, Y. Su, H. Zhang, Z. Ouyang, Chang’E-4 initial spectroscopic identification of lunar far-side mantle-derived materials. Nature 569, 378–382 (2019). https://doi.org/10.1038/s41586-019-1189-0
J. Liu, M. Touboul, A. Ishikawa, R.J. Walker, D. Graham Pearson, Widespread tungsten isotope anomalies and W mobility in crustal and mantle rocks of the Eoarchean Saglek Block, northern Labrador, Canada: implications for early Earth processes and W recycling. Earth Planet. Sci. Lett. 448, 13–23 (2016). https://doi.org/10.1016/j.epsl.2016.05.001
S.J. Lock, S.T. Stewart, The structure of terrestrial bodies: impact heating, corotation limits, and synestias. J. Geophys. Res., Planets 122(5), 950–982 (2017). https://doi.org/10.1002/2016JE005239
S.J. Lock, S.T. Stewart, Giant impacts stochastically change the internal pressures of terrestrial planets. Sci. Adv. 5(9), eaav3746 (2019). https://doi.org/10.1126/sciadv.aav3746
S.J. Lock, S.T. Stewart, M.I. Petaev, Z. Leinhardt, M.T. Mace, S.B. Jacobsen, M. Ćuk, The origin of the moon within a terrestrial synestia. J. Geophys. Res., Planets 123(4), 910–951 (2018). https://doi.org/10.1002/2017JE005333
S.J. Lock, S.T. Stewart, M. Ćuk, The energy budget and figure of Earth during recovery from the Moon-forming giant impact. Earth Planet. Sci. Lett. 530, 115,885 (2020). https://doi.org/10.1016/j.epsl.2019.115885
J. Longhi, Petrogenesis of picritic mare magmas: constraints on the extent of early lunar differentiation. Geochim. Cosmochim. Acta 70(24), 5919–5934 (2006). https://doi.org/10.1016/j.gca.2006.09.023
G.W. Lugmair, R.W. Carlson, The Sm-Nd history of KREEP, in Lunar and Planetary Science Conference Abstracts, vol. 9 (1978), pp. 689–704
G. Lugmair, A. Shukolyukov, Early solar system timescales according to 53Mn-53Cr systematics. Geochim. Cosmochim. Acta 62(16), 2863–2886 (1998). https://doi.org/10.1016/S0016-7037(98)00189-6
C. Maas, U. Hansen, Dynamics of a terrestrial magma ocean under planetary rotation: a study in spherical geometry. Earth Planet. Sci. Lett. 513, 81–94 (2019). https://doi.org/10.1016/j.epsl.2019.02.016
S. Marchi, R.M. Canup, R.J. Walker, Heterogeneous delivery of silicate and metal to the Earth by large planetesimals. Nat. Geosci. 11(1), 77–81 (2018). https://doi.org/10.1038/s41561-017-0022-3
N.E. Marks, L.E. Borg, C.K. Shearer, W.S. Cassata, Geochronology of an Apollo 16 clast provides evidence for a basin-forming impact 4.3 billion years ago. J. Geophys. Res., Planets 124(10), 2465–2481 (2019). https://doi.org/10.1029/2019JE005966
T.K. Mayeda, R.N. Clayton, Oxygen isotopic compositions of Aubrites and some unique meteorites. Geochim. Cosmochim. Acta 14(2), 1145–1151 (1980)
T.K. Mayeda, R.N. Clayton, Oxygen isotopic composition of ALHA 81005, in Lunar and Planetary Science Conference Abstracts, vol. 14 (1983), p. 472
K.T. Mayeda, N.R. Clayton, Oxygen isotopic compositions of unique Antarctic meteorites. Proc. NIPR Symp. Antarct. Meteor. 14, 172 (1989a)
T.K. Mayeda, R.N. Clayton, Oxygen isotopes in the Bholghati Howardite, in Lunar and Planetary Science Conference Abstracts, vol. 20 (1989b), p. 648
T. Mayeda, R. Clayton, K. Yanai, Oxygen isotopic compositions of several Antarctic meteorites. Mem. Natl. Inst. Polar Res., Spec. Issue 46, 144–150 (1987)
T.K. Mayeda, K. Yanai, R.N. Clayton, Another martian meteorite, in Lunar and Planetary Science Conference Abstracts, vol. 26 (1995), pp. 917–918
T.J. McCoy, K. Keil, D.D. Bogard, D.H. Garrison, I. Casanova, M.M. Lindstrom, A.J. Brearley, K. Kehm, R.H. Nichols, C.M. Hohenberg, Origin and history of impact-melt rocks of enstatite chondrite parentage. Geochim. Cosmochim. Acta 59(1), 161–175 (1995). https://doi.org/10.1016/0016-7037(94)00231-A
T.J. McCoy, K. Keil, R.N. Clayton, T.K. Mayeda, D.D. Bogard, D.H. Garrison, G.R. Huss, I.D. Hutcheon, R. Wieler, A petrologic, chemical, and isotopic study of Monument Draw and comparison with other acapulcoites: evidence for formation by incipient partial melting. Geochim. Cosmochim. Acta 60(14), 2681–2708 (1996). https://doi.org/10.1016/0016-7037(96)00109-3
T.J. McCoy, K. Keil, R.N. Clayton, T.K. Mayeda, D.D. Bogard, D.H. Garrison, R. Wieler, A petrologic and isotopic study of lodranites: evidence for early formation as partial melt residues from heterogeneous precursors. Geochim. Cosmochim. Acta 61(3), 623–637 (1997). https://doi.org/10.1016/S0016-7037(96)00359-6
W. McDonough, S. Sun, The composition of the Earth. Chem. Geol. 120(3–4), 223–253 (1995). https://doi.org/10.1016/0009-2541(94)00140-4
C.L. McLeod, A.D. Brandon, R.M.G. Armytage, Constraints on the formation age and evolution of the Moon from 142Nd-143Nd systematics of Apollo 12 basalts. Earth Planet. Sci. Lett. 396, 179–189 (2014). https://doi.org/10.1016/j.epsl.2014.04.007
F. Meissner, W.D. Schmidt-Ott, L. Ziegeler, Half-life and \(\alpha \)-ray energy of 146Sm. Eur. Phys. J. A 327(2), 171–174 (1987). https://doi.org/10.1007/BF01292406
H.J. Melosh, New approaches to the Moon’s isotopic crisis. Philos. Trans. R. Soc. A, Math. Phys. Eng. Sci. 372(2024), 20130 (2014). https://doi.org/10.1098/rsta.2013.0168. 168
Y. Miyazaki, J. Korenaga, On the timescale of magma ocean solidification and its chemical consequences: 2. Compositional differentiation under crystal accumulation and matrix compaction. J. Geophys. Res., Solid Earth 124(4), 3399–3419 (2019). https://doi.org/10.1029/2018JB016928
A. Morbidelli, B. Wood, Late accretion and the late veneer, in The Early Earth: Accretion and Differentiation, ed. by J. Badro, M. Walter (John Wiley & Sons, Inc., Hoboken, 2014). Chap. 4. https://doi.org/10.1002/9781118860359.ch4
J.W. Morgan, Osmium isotope constraints on Earth’s late accretionary history. Nature 317(6039), 703–705 (1985). https://doi.org/10.1038/317703a0
J.W. Morgan, J. Hertogen, E. Anders, The Moon: composition determined by nebular processes. Moon Planets 18(4), 465–478 (1978). https://doi.org/10.1007/BF00897296
L.V. Moroz, V.I. Ustinov, N.N. Kononkova, N.I. Zaslavskaya, Y.A. Shukolyukov, Oxygen isotopes of chromite and chemical composition of the minerals from polymineral nodules in Sikhote-Alin meteorite, in Lunar and Planetary Science Conference Abstracts, vol. 19 (1988), pp. 809–810
B. Mougel, F. Moynier, C. Göpel, Chromium isotopic homogeneity between the Moon, the Earth, and enstatite chondrites. Earth Planet. Sci. Lett. 481, 1–8 (2018). https://doi.org/10.1016/j.epsl.2017.10.018
S. Mukhopadhyay, Early differentiation and volatile accretion recorded in deep-mantle neon and xenon. Nature 486(7401), 101–104 (2012). https://doi.org/10.1038/nature11141
S. Mukhopadhyay, R. Parai, Noble gases: a record of Earth’s evolution and mantle dynamics. Annu. Rev. Earth Planet. Sci. 47(1), 389–419 (2019). https://doi.org/10.1146/annurev-earth-053018-060238
A. Mundl, M. Touboul, M.G. Jackson, J.M.D. Day, M.D. Kurz, V. Lekic, R.T. Helz, R.J. Walker, Tungsten-182 heterogeneity in modern ocean island basalts. Science 356(6333), 66–69 (2017). https://doi.org/10.1126/science.aal4179
A. Mundl, R.J. Walker, J.R. Reimink, R.L. Rudnick, R.M. Gaschnig, Tungsten-182 in the upper continental crust: evidence from glacial diamictites. Chem. Geol. 494, 144–152 (2018). https://doi.org/10.1016/j.chemgeo.2018.07.036
A. Mundl-Petermeier, R.J. Walker, R.A. Fischer, V. Lekic, M.G. Jackson, M.D. Kurz, Anomalous 182W in high 3He/4He ocean island basalts: fingerprints of Earth’s core? Geochim. Cosmochim. Acta 271, 194–211 (2020). https://doi.org/10.1016/j.gca.2019.12.020
M. Nakajima, D.J. Stevenson, Investigation of the initial state of the Moon-forming disk: bridging SPH simulations and hydrostatic models. Icarus 233, 259–267 (2014). https://doi.org/10.1016/j.icarus.2014.01.008
M. Nakajima, D.J. Stevenson, Melting and mixing states of the Earth’s mantle after the Moon-forming impact. Earth Planet. Sci. Lett. 427, 286–295 (2015). https://doi.org/10.1016/j.epsl.2015.06.023
C.E. Nehru, M. Prinz, M.K. Weisberg, M.E. Ebihara, R.N. Clayton, T.K. Mayeda, A new Brachinite and petrogenesis of the group, in Lunar and Planetary Science Conference Abstracts, vol. 27 (1996), pp. 943–944
A. Nemchin, N. Timms, R. Pidgeon, T. Geisler, S. Reddy, C. Meyer, Timing of crystallization of the lunar magma ocean constrained by the oldest zircon. Nat. Geosci. 2(2), 133–136 (2009). https://doi.org/10.1038/ngeo417
P. Ni, Y. Zhang, S. Chen, J. Gagnon, A melt inclusion study on volatile abundances in the lunar mantle. Geochim. Cosmochim. Acta 249, 17–41 (2019). https://doi.org/10.1016/j.gca.2018.12.034
N.X. Nie, N. Dauphas, Vapor drainage in the protolunar disk as the cause for the depletion in volatile elements of the Moon. Astrophys. J. 884(2), L48 (2019). https://doi.org/10.3847/2041-8213/ab4a16
M.D. Norman, L.E. Borg, L.E. Nyquist, D.D. Bogard, Chronology, geochemistry, and petrology of a ferroan noritic anorthosite clast from Descartes breccia 67215: clues to the age, origin, structure, and impact history of the lunar crust. Meteorit. Planet. Sci. 38(4), 645–661 (2003). https://doi.org/10.1111/j.1945-5100.2003.tb00031.x
L.E. Nyquist, H. Wiesmann, B. Bansal, C.Y. Shih, J.E. Keith, C.L. Harper, 146Sm-142Nd formation interval for the lunar mantle. Geochim. Cosmochim. Acta 59(13), 2817–2837 (1995). https://doi.org/10.1016/0016-7037(95)00175-Y
L.E. Nyquist, C.Y. Shih, Y.D. Reese, J. Park, D.D. Bogard, D.H. Garrison, A. Yamaguchi, Lunar crustal history recorded in lunar anorthosites, in Lunar and Planetary Science Conference, vol. 41 (2010), p. 1383
E.J. Olsen, B.D. Dod, R.A. Schmitt, P.P. Sipiera, Monticello: a class-rich Howardite. Meteoritics 22(1), 81–96 (1987). https://doi.org/10.1111/j.1945-5100.1987.tb00885.x
E. Olsen, A. Davis, R.S. Clarke, L. Schultz, H.W. Weber, R. Clayton, T. Mayeda, E. Jarosewich, P. Sylvester, L. Grossman, M.S. Wang, M.E. Lipschutz, I.M. Steele, J. Schwade, Watson: a new link in the HE iron chain. Meteoritics 29(2), 200–213 (1994). https://doi.org/10.1111/j.1945-5100.1994.tb00672.x
J. O’Neil, R.W. Carlson, D. Francis, R.K. Stevenson, C.M. Deibel, B. DiGiovine, J.P. Greene, D.J. Henderson, C.L. Jiang, S.T. Marley, T. Nakanishi, R.C. Pardo, K.E. Rehm, D. Robertson, R. Scott, C. Schmitt, X.D. Tang, R. Vondrasek, A. Yokoyama, Neodymium-142 evidence for Hadean mafic crust. Science 321(5897), 1828–1831 (2008). https://doi.org/10.1126/science.1161925
N. Onuma, R. Clayton, T. Mayeda, K. Yanai, Oxygen isotopes in several Yamato meteorites. Mem. Natl. Inst. Polar Res., Spec. Issue 8, 220–224 (1978)
N. Onuma, Y. Ikeda, T.K. Mayeda, R.N. Clayton, K. Yanai, Oxygen isotopic composition of photographically described inclusions from Antarctic unequilibrated ordinary chondrites, in Memoirs of National Institute of Polar Research. Special Issue, vol. 30 (1983), pp. 306–314
K. Pahlevan, D.J. Stevenson, Equilibration in the aftermath of the lunar-forming giant impact. Earth Planet. Sci. Lett. 262(3–4), 438–449 (2007). https://doi.org/10.1016/j.epsl.2007.07.055
R.C. Paniello, J.M.D. Day, F. Moynier, Zinc isotopic evidence for the origin of the Moon. Nature 490(7420), 376–379 (2012). https://doi.org/10.1038/nature11507
R. Parai, S. Mukhopadhyay, The evolution of MORB and plume mantle volatile budgets: constraints from fission Xe isotopes in Southwest Indian Ridge basalts. Geochem. Geophys. Geosyst. 16(3), 719–735 (2015). https://doi.org/10.1002/2014GC005566
R. Parai, S. Mukhopadhyay, J. Standish, Heterogeneous upper mantle Ne, Ar and Xe isotopic compositions and a possible Dupal noble gas signature recorded in basalts from the Southwest Indian Ridge. Earth Planet. Sci. Lett. 359–360, 227–239 (2012). https://doi.org/10.1016/j.epsl.2012.10.017
R. Parai, S. Mukhopadhyay, J.M. Tucker, M.K. Pető, The emerging portrait of an ancient, heterogeneous and continuously evolving mantle plume source. Lithos 346–347, 105,153 (2019). https://doi.org/10.1016/j.lithos.2019.105153
M.I. Petaev, V.I. Ustinov, N.I. Zaslavkaya, E.Y. Gavrilov, A. Shukolyukov, Oxygen isotopes in Pomozdino meteorite, in Lunar and Planetary Science Conference Abstracts, vol. 19 (1988), p. 917
B.J. Peters, R.W. Carlson, J.M. Day, M.F. Horan, Hadean silicate differentiation preserved by anomalous 142Nd/144Nd ratios in the Réunion hotspot source. Nature 555(7694), 89–93 (2018). https://doi.org/10.1038/nature25754
M.K. Pető, S. Mukhopadhyay, K.A. Kelley, Heterogeneities from the first 100 million years recorded in deep mantle noble gases from the Northern Lau Back-arc Basin. Earth Planet. Sci. Lett. 369–370, 13–23 (2013). https://doi.org/10.1016/j.epsl.2013.02.012
D. Porcelli, D. Woolum, P. Cassen, Deep Earth rare gases: initial inventories, capture from the solar nebula, and losses during moon formation. Earth Planet. Sci. Lett. 193(1–2), 237–251 (2001). https://doi.org/10.1016/S0012-821X(01)00493-9
N.J. Potts, J.J. Barnes, R. Tartèse, I.A. Franchi, M. Anand, Chlorine isotopic compositions of apatite in Apollo 14 rocks: evidence for widespread vapor-phase metasomatism on the lunar nearside \(\sim4\) billion years ago. Geochim. Cosmochim. Acta 230, 46–59 (2018). https://doi.org/10.1016/j.gca.2018.03.022
E.A. Pringle, F. Moynier, Rubidium isotopic composition of the Earth, meteorites, and the Moon: evidence for the origin of volatile loss during planetary accretion. Earth Planet. Sci. Lett. 473, 62–70 (2017). https://doi.org/10.1016/j.epsl.2017.05.033
M. Prinz, N. Chatterjee, M.K. Weisberg, R.N. Clayton, T.K. Mayeda, MAC88177: a new type of achondrite? in Lunar and Planetary Science Conference Abstracts, vol. 22 (1991), p. 1099
I. Puchtel, M. Humayun, Platinum group elements in Kostomuksha komatiites and basalts: implications for oceanic crust recycling and core-mantle interaction. Geochim. Cosmochim. Acta 64(24), 4227–4242 (2000). https://doi.org/10.1016/S0016-7037(00)00492-0
I.S. Puchtel, J. Blichert-Toft, M. Touboul, M.F. Horan, R.J. Walker, The coupled 182W-142Nd record of early terrestrial mantle differentiation. Geochem. Geophys. Geosyst. 17(6), 2168–2193 (2016). https://doi.org/10.1002/2016GC006324
I.S. Puchtel, J. Blichert-Toft, M. Touboul, R.J. Walker, 182W and HSE constraints from 2.7 Ga komatiites on the heterogeneous nature of the Archean mantle. Geochim. Cosmochim. Acta 228, 1–26 (2018). https://doi.org/10.1016/j.gca.2018.02.030
A. Pun, K. Keil, G.J. Taylor, E. King, A unique Eucrite clast from the Kapoeta Howardite, in Lunar and Planetary Science Conference Abstracts, vol. 22 (1991), p. 1105
L. Qin, C.M. Alexander, R.W. Carlson, M.F. Horan, T. Yokoyama, Contributors to chromium isotope variation of meteorites. Geochim. Cosmochim. Acta 74(3), 1122–1145 (2010a). https://doi.org/10.1016/j.gca.2009.11.005
L. Qin, D. Rumble, C.M. Alexander, R.W. Carlson, P. Jenniskens, M.H. Shaddad, The chromium isotopic composition of Almahata Sitta. Meteorit. Planet. Sci. 45(10–11), 1771–1777 (2010b). https://doi.org/10.1111/j.1945-5100.2010.01109.x
E.V. Quintana, T. Barclay, W.J. Borucki, J.F. Rowe, J.E. Chambers, The frequency of giant impacts on Earth-like worlds. Astrophys. J. 821(2), 126 (2016). https://doi.org/10.3847/0004-637X/821/2/126
S. Recca, E. Scott, K. Keil, R. Clayton, T. Mayeda, G. Huss, E. Jarosewich, K. Weeks, F. Hasan, D. Sears, R. Wieler, P. Signer, Ragland, an LL3.4 chondrite find from New Mexico. Meteoritics 21(2), 217–229 (1986). https://doi.org/10.1111/j.1945-5100.1986.tb01243.x
J.R. Reimink, T. Chacko, R.W. Carlson, S.B. Shirey, J. Liu, R.A. Stern, A.M. Bauer, D.G. Pearson, L.M. Heaman, Petrogenesis and tectonics of the Acasta Gneiss Complex derived from integrated petrology and 142Nd and 182W extinct nuclide-geochemistry. Earth Planet. Sci. Lett. 494, 12–22 (2018). https://doi.org/10.1016/j.epsl.2018.04.047
A. Reufer, M.M. Meier, W. Benz, R. Wieler, A hit-and-run giant impact scenario. Icarus 221(1), 296–299 (2012). https://doi.org/10.1016/j.icarus.2012.07.021
A.E. Ringwood, Origin of the Earth and Moon (Springer, New York, 1979)
A.E. Ringwood, Terrestrial origin of the Moon. Nature 322(6077), 323–328 (1986). https://doi.org/10.1038/322323a0
A.E. Ringwood, S.E. Kesson, Basaltic magmatism and the bulk composition of the Moon. Moon 16(4), 425–464 (1977). https://doi.org/10.1007/BF00577902
A. Ringwood, S. Seifert, H. Wänke, A komatiite component in Apollo 16 highland breccias: implications for the nickel-cobalt systematics and bulk composition of the moon. Earth Planet. Sci. Lett. 81(2–3), 105–117 (1987). https://doi.org/10.1016/0012-821X(87)90149-X
H. Rizo, M. Boyet, J. Blichert-Toft, M. Rosing, Combined Nd and Hf isotope evidence for deep-seated source of Isua lavas. Earth Planet. Sci. Lett. 312(3–4), 267–279 (2011). https://doi.org/10.1016/j.epsl.2011.10.014
H. Rizo, R. Walker, R. Carlson, M. Touboul, M. Horan, I. Puchtel, M. Boyet, M. Rosing, Early Earth differentiation investigated through 142Nd, 182W, and highly siderophile element abundances in samples from Isua, Greenland. Geochim. Cosmochim. Acta 175, 319–336 (2016a). https://doi.org/10.1016/j.gca.2015.12.007
H. Rizo, R.J. Walker, R.W. Carlson, M.F. Horan, S. Mukhopadhyay, V. Manthos, D. Francis, M.G. Jackson, Preservation of Earth-forming events in the tungsten isotopic composition of modern flood basalts. Science 352(6287), 809–812 (2016b). https://doi.org/10.1126/science.aad8563
H. Rizo, D. Andrault, N.R. Bennett, M. Humayun, A. Brandon, I. Vlastelic, B. Moine, A. Poirier, M.A. Bouhifd, D.T. Murphy, 182W evidence for core-mantle interaction in the source of mantle plumes. Geochem. Perspect. Lett. 11, 6–11 (2019). https://doi.org/10.7185/geochemlet.1917
C.S. Romanek, E.C. Perry, A.H. Treiman, R.A. Socki, J.H. Jones, E.K. Gibson, Oxygen isotopic record of silicate alteration in the Shergotty-Nakhla-Chassigny meteorite Lafayette. Meteorit. Planet. Sci. 33(4), 775–784 (1998). https://doi.org/10.1111/j.1945-5100.1998.tb01683.x
M.W. Rowe, R.N. Clayton, T.K. Mayeda, Oxygen isotopes in separated components of CI and CM meteorites. Geochim. Cosmochim. Acta 58(23), 5341–5347 (1994). https://doi.org/10.1016/0016-7037(94)90317-4
R. Rufu, O. Aharonson, Impact dynamics of moons within a planetary potential. J. Geophys. Res., Planets 124(4), 1008–1019 (2019). https://doi.org/10.1029/2018JE005798
R. Rufu, O. Aharonson, H.B. Perets, A multiple-impact origin for the Moon. Nat. Geosci. 10, 89–94 (2017). https://doi.org/10.1038/ngeo2866
S.S. Russell, T.J. McCoy, E. Jarosewich, R.D. Ash, The Burnwell, Kentucky, low iron oxide chondrite fall: description, classification and origin. Meteorit. Planet. Sci. 33(4), 853–856 (1998). https://doi.org/10.1111/j.1945-5100.1998.tb01691.x
S.S. Russell, M.E. Zolensky, K. Righter, L. Folco, R.H. Jones, H.C. Connolly, M.M. Grady, J.N. Grossman, The Meteoritical Bulletin, No. 89, 2005 September. Meteorit. Planet. Sci. 40(S9), A201–A263 (2005). https://doi.org/10.1111/j.1945-5100.2005.tb00425.x
A. Ruzicka, D.A. Kring, D.H. Hill, W.V. Boynton, R.N. Clayton, T.K. Mayeda, Silica-rich orthopyroxenite in the Bovedy chondrite. Meteoritics 30(1), 57–70 (1995). https://doi.org/10.1111/j.1945-5100.1995.tb01212.x
J. Salmon, R.M. Canup, Lunar accretion from a Roche-interior fluid disk. Astrophys. J. 760(1), 83 (2012). https://doi.org/10.1088/0004-637X/760/1/83
J. Salmon, R.M. Canup, Accretion of the Moon from non-canonical discs. Philos. Trans. R. Soc. A, Math. Phys. Eng. Sci. 372(2024), 20130,256 (2014). https://doi.org/10.1098/rsta.2013.0256
P. Saxena, L. Elkins-Tanton, N. Petro, A. Mandell, A model of the primordial lunar atmosphere. Earth Planet. Sci. Lett. 474, 198–205 (2017). https://doi.org/10.1016/j.epsl.2017.06.031
M. Schiller, E. Van Kooten, J.C. Holst, M.B. Olsen, M. Bizzarro, Precise measurement of chromium isotopes by MC-ICPMS. J. Anal. At. Spectrom. 29(8), 1406–1416 (2014). https://doi.org/10.1039/c4ja00018h
R. Schoenberg, S. Zink, M. Staubwasser, F. von Blanckenburg, The stable Cr isotope inventory of solid Earth reservoirs determined by double spike MC-ICP-MS. Chem. Geol. 249(3–4), 294–306 (2008). https://doi.org/10.1016/J.CHEMGEO.2008.01.009
H. Schulze, A. Bischoff, H. Palme, B. Spettel, G. Dreibus, J. Otto, Mineralogy and chemistry of Rumuruti: the first meteorite fall of the new R chondrite group. Meteoritics 29(2), 275–286 (1994). https://doi.org/10.1111/j.1945-5100.1994.tb00681.x
D.W.G. Sears, J.D. Batchelor, B. Mason, E.R.D. Scott, R.N. Clayton, T.K. Mayeda, South Australian type 3 chondrites. Meteoritics 25(4), 407–408 (1990). https://doi.org/10.1111/j.1945-5100.1990.tb00722.x
S. Seifert, A. E. Ringwood, The lunar geochemistry of chromium and vanadium. Earth Moon Planets 40(1), 45–70 (1988). https://doi.org/10.1007/BF00057946
K. Shariff, Fluid mechanics in disks around young stars. Annu. Rev. Fluid Mech. 41(1), 283–315 (2009). https://doi.org/10.1146/annurev.fluid.010908.165144
Z.D. Sharp, C.K. Shearer, K.D. McKeegan, J.D. Barnes, Y.Q. Wang, The chlorine isotope composition of the Moon and implications for an anhydrous mantle. Science 329(5995), 1050–1053 (2010). https://doi.org/10.1126/science.1192606
Z.D. Sharp, J.A. Mercer, R.H. Jones, A.J. Brearley, J. Selverstone, A. Bekker, T. Stachel, The chlorine isotope composition of chondrites and Earth. Geochim. Cosmochim. Acta 107, 189–204 (2013). https://doi.org/10.1016/j.gca.2013.01.003
C.K. Shearer, K. Righter, Behavior of tungsten and hafnium in silicates: a crystal chemical basis for understanding the early evolution of the terrestrial planets. Geophys. Res. Lett. 30(1), 7-1–7-4 (2003). https://doi.org/10.1029/2002gl015523
A. Shukolyukov, G. Lugmair, Manganese–chromium isotope systematics of carbonaceous chondrites. Earth Planet. Sci. Lett. 250(1–2), 200–213 (2006a). https://doi.org/10.1016/J.EPSL.2006.07.036
A. Shukolyukov, G.W. Lugmair, The Mn-Cr isotope systematics in the ureilites Kenna and LEW85440, in Lunar and Planetary Science Conference Abstracts, vol. 37 (2006b), p. 1478
A. Shukolyukov, G.W. Lugmair, A.J. Irving, Mn-Cr isotope systematics of angrite Northwest Africa 4801, in Lunar and Planetary Science Conference Abstracts, vol. 40 (2009), p. 1381
S.B. Simon, L. Grossman, I. Casanova, S. Symes, P. Benoit, D.W.G. Sears, J.F. Wacker, Axtell, a new CV3 chondrite find from Texas. Meteoritics 30(1), 42–46 (1995). https://doi.org/10.1111/j.1945-5100.1995.tb01210.x
C.K. Sio, L.E. Borg, W.S. Cassata, The timing of lunar solidification and mantle overturn recorded in ferroan anorthosite 62237. Earth Planet. Sci. Lett. 538, 116,219 (2020). https://doi.org/10.1016/j.epsl.2020.116219
G.A. Snyder, C.R. Neal, L.A. Taylor, A.N. Halliday, Processes involved in the formation of magnesian-suite plutonic rocks from the highlands of the Earth’s Moon. J. Geophys. Res. 100(E5), 9365–9388 (1995). https://doi.org/10.1029/95JE00575
V.S. Solomatov, D.J. Stevenson, Kinetics of crystal growth in a terrestrial magma ocean. J. Geophys. Res. 98(E3), 5407 (1993a). https://doi.org/10.1029/92JE02839
V.S. Solomatov, D.J. Stevenson, Nonfractional crystallization of a terrestrial magma ocean. J. Geophys. Res. 98(E3), 5391–5406 (1993b). https://doi.org/10.1029/92JE02579
V.S. Solomatov, D.J. Stevenson, Suspension in convective layers and style of differentiation of a terrestrial magma ocean. J. Geophys. Res. 98(E3), 5375 (1993c). https://doi.org/10.1029/92JE02948
P.A. Sossi, F. Moynier, Chemical and isotopic kinship of iron in the Earth and Moon deduced from the lunar Mg-Suite. Earth Planet. Sci. Lett. 471, 125–135 (2017). https://doi.org/10.1016/j.epsl.2017.04.029
P.A. Sossi, F. Moynier, K. van Zuilen, Volatile loss following cooling and accretion of the Moon revealed by chromium isotopes. Proc. Natl. Acad. Sci. 115(43), 10,920–10,925 (2018). https://doi.org/10.1073/pnas.1809060115
P.A. Sossi, S. Klemme, H.S.C. O’Neill, J. Berndt, F. Moynier, Evaporation of moderately volatile elements from silicate melts: experiments and theory. Geochim. Cosmochim. Acta 260, 204–231 (2019). https://doi.org/10.1016/j.gca.2019.06.021
P. Sprung, T. Kleine, E.E. Scherer, Isotopic evidence for chondritic Lu/Hf and Sm/Nd of the Moon. Earth Planet. Sci. Lett. 380, 77–87 (2013). https://doi.org/10.1016/j.epsl.2013.08.018
E.S. Steenstra, N. Rai, J.S. Knibbe, Y.H. Lin, W. van Westrenen, New geochemical models of core formation in the Moon from metal-silicate partitioning of 15 siderophile elements. Earth Planet. Sci. Lett. 441, 1–9 (2016). https://doi.org/10.1016/j.epsl.2016.02.028
E.S. Steenstra, Y. Lin, D. Dankers, N. Rai, J. Berndt, S. Matveev, W. van Westrenen, The lunar core can be a major reservoir for volatile elements S, Se, Te and Sb. Sci. Rep. 14, 552 (2017). https://doi.org/10.1038/s41598-017-15203-0
E.S. Steenstra, J. Berndt, S. Klemme, Y. Fei, W. van Westrenen, A possible high-temperature origin of the Moon and its geochemical consequences. Earth Planet. Sci. Lett. 538, 116,222 (2020). https://doi.org/10.1016/j.epsl.2020.116222
A. Stephant, M. Anand, X. Zhao, Q.H. Chan, M. Bonifacie, I.A. Franchi, The chlorine isotopic composition of the Moon: insights from melt inclusions. Earth Planet. Sci. Lett. 523, 115,715 (2019). https://doi.org/10.1016/j.epsl.2019.115715
M. Stepniewski, J. Borucki, J. Siemiatkowski, New data on the L5(S1) chondrite Baszkowka (Poland). Meteorit. Planet. Sci. 33, A150–A151 (1998)
R. Tartèse, M. Anand, K.H. Joy, I.A. Franchi, H and Cl isotope systematics of apatite in brecciated lunar meteorites Northwest Africa 4472, Northwest Africa 773, Sayh al Uhaymir 169, and Kalahari 009. Meteorit. Planet. Sci. 49(12), 2266–2289 (2014). https://doi.org/10.1111/maps.12398
S.R. Taylor, Planetary Science: A Lunar Perspective (Lunar and Planetary Institute, Houston, 1982)
S.R. Taylor, The Moon re-examined. Geochim. Cosmochim. Acta 141, 670–676 (2014). https://doi.org/10.1016/j.gca.2014.06.031
S.R. Taylor, S. McLennan, Planetary Crusts: Their Composition, Origin and Evolution (Cambridge University Press, Cambridge, 2009)
G.J. Taylor, M.A. Wieczorek, Lunar bulk chemical composition: a post-Gravity Recovery and Interior Laboratory reassessment. Philos. Trans. R. Soc. A, Math. Phys. Eng. Sci. 372(2024), 20130,242 (2014). https://doi.org/10.1098/rsta.2013.0242
D.J. Taylor, K.D. McKeegan, T.M. Harrison, Lu-Hf zircon evidence for rapid lunar differentiation. Earth Planet. Sci. Lett. 279(3–4), 157–164 (2009). https://doi.org/10.1016/j.epsl.2008.12.030
M.M. Thiemens, P. Sprung, R.O. Fonseca, F.P. Leitzke, C. Münker, Early Moon formation inferred from hafnium–tungsten systematics. Nat. Geosci. 12(9), 696–700 (2019). https://doi.org/10.1038/s41561-019-0398-3
C. Thompson, D.J. Stevenson, Gravitational instability in two-phase disks and the origin of the Moon. Astrophys. J. 333, 452 (1988). https://doi.org/10.1086/166760
Z. Tian, J. Wisdom, L. Elkins-Tanton, Coupled orbital-thermal evolution of the early Earth-Moon system with a fast-spinning Earth. Icarus 281, 90–102 (2017). https://doi.org/10.1016/j.icarus.2016.08.030
M. Touboul, I.S. Puchtel, R.J. Walker, 182W evidence for long-term preservation of early mantle differentiation products. Science 335(6072), 1065–1069 (2012). https://doi.org/10.1126/science.1216351
M. Touboul, J. Liu, J. O’Neil, I.S. Puchtel, R.J. Walker, New insights into the Hadean mantle revealed by 182W and highly siderophile element abundances of supracrustal rocks from the Nuvvuagittuq Greenstone Belt, Quebec, Canada. Chem. Geol. 383, 63–75 (2014). https://doi.org/10.1016/j.chemgeo.2014.05.030
M. Touboul, I.S. Puchtel, R.J. Walker, Tungsten isotopic evidence for disproportional late accretion to the Earth and Moon. Nature 520, 530–533 (2015). https://doi.org/10.1038/nature14355
A.H. Treiman, J.W. Boyce, J. Gross, Y. Guan, J.M. Eiler, E.M. Stolper, Phosphate-halogen metasomatism of lunar granulite 79215: impact-induced fractionation of volatiles and incompatible elements. Am. Mineral. 99(10), 1860–1870 (2014). https://doi.org/10.2138/am-2014-4822
A. Trinquier, J. Birck, C.J. Allegre, Widespread 54Cr heterogeneity in the inner solar system. Astrophys. J. 655(2), 1179–1185 (2007). https://doi.org/10.1086/510360
A. Trinquier, T. Elliott, D. Ulfbeck, C. Coath, A.N. Krot, M. Bizzarro, Origin of nucleosynthetic isotope heterogeneity in the solar protoplanetary disk. Science 324(5925), 374–376 (2009). https://doi.org/10.1126/science.1168221
J.M. Tucker, S. Mukhopadhyay, Evidence for multiple magma ocean outgassing and atmospheric loss episodes from mantle noble gases. Earth Planet. Sci. Lett. 393, 254–265 (2014). https://doi.org/10.1016/j.epsl.2014.02.050
J.M. Tucker, S. Mukhopadhyay, J.G. Schilling, The heavy noble gas composition of the depleted MORB mantle (DMM) and its implications for the preservation of heterogeneities in the mantle. Earth Planet. Sci. Lett. 355–356, 244–254 (2012). https://doi.org/10.1016/j.epsl.2012.08.025
J.W. Valley, A.J. Cavosie, T. Ushikubo, D.A. Reinhard, D.F. Lawrence, D.J. Larson, P.H. Clifton, T.F. Kelly, S.A. Wilde, D.E. Moser, M.J. Spicuzza, Hadean age for a post-magma-ocean zircon confirmed by atom-probe tomography. Nat. Geosci. 7(3), 219–223 (2014). https://doi.org/10.1038/ngeo2075
C. Vockenhuber, F. Oberli, M. Bichler, I. Ahmad, G. Quitté, M. Meier, A.N. Halliday, D.C. Lee, W. Kutschera, P. Steier, R.J. Gehrke, R.G. Helmer, New half-life measurement of 182Hf: improved chronometer for the early solar system. Phys. Rev. Lett. 172, 501 (2004). https://doi.org/10.1103/PhysRevLett.93.172501
R.J. Walker, Highly siderophile elements in the Earth, Moon and Mars: update and implications for planetary accretion and differentiation. Chem. Erde 69(2), 101–125 (2009). https://doi.org/10.1016/j.chemer.2008.10.001
K. Wang, S.B. Jacobsen, Potassium isotopic evidence for a high-energy giant impact origin of the Moon. Nature 538(7626), 487–490 (2016). https://doi.org/10.1038/nature19341
X. Wang, Q. Amet, C. Fitoussi, B. Bourdon, Tin isotope fractionation during magmatic processes and the isotope composition of the bulk silicate Earth. Geochim. Cosmochim. Acta 228, 320–335 (2018). https://doi.org/10.1016/j.gca.2018.02.014
X. Wang, C. Fitoussi, B. Bourdon, B. Fegley, S. Charnoz, Tin isotopes indicative of liquid–vapour equilibration and separation in the Moon-forming disk. Nat. Geosci. 12(9), 707–711 (2019a). https://doi.org/10.1038/s41561-019-0433-4
Y. Wang, W. Hsu, Y. Guan, An extremely heavy chlorine reservoir in the Moon: insights from the apatite in lunar meteorites. Sci. Rep. 9(1), 5727 (2019b). https://doi.org/10.1038/s41598-019-42224-8
H. Wänke, G. Dreibus, Chemical composition and isotopic evidence for the early history of the Earth-Moon system, in Tidal Friction and the Earth’s Rotation II, ed. by P. Brosche, J. Sündermann (Springer, Berlin, 1982), pp. 322–344
H. Wänke, H. Baddenhausen, K. Blum, M. Cendales, G. Dreibus, H. Hofmeister, H. Kruse, E. Jagoutz, C. Palme, B. Spettel, On the chemistry of lunar samples and achondrites - primary matter in the lunar highlands: a re-evaluation, in Lunar and Planetary Science Conference Abstracts, vol. 2 (1977a), pp. 2191–2213
H. Wanke, H. Palme, H. Baddenhausen, G. Dreibus, H. Kruse, B. Spettel, Element correlations and the bulk composition of the Moon. Philos. Trans. R. Soc. A, Math. Phys. Eng. Sci. 285(1327), 41–48 (1977b). https://doi.org/10.1098/rsta.1977.0041
W.R. Ward, Evolution of a protolunar disk in vapor/melt equilibrium. J. Geophys. Res., Planets 122(2), 342–357 (2017). https://doi.org/10.1002/2016JE005198
P.H. Warren, The magma ocean concept and lunar evolution. Annu. Rev. Earth Planet. Sci. 13(1), 201–240 (1985). https://doi.org/10.1146/annurev.ea.13.050185.001221
P.H. Warren, “New” lunar meteorites: implications for composition of the global lunar surface, lunar crust, and the bulk Moon. Meteorit. Planet. Sci. 40(3), 477–506 (2005). https://doi.org/10.1111/j.1945-5100.2005.tb00395.x
D. Weber, R.N. Clayton, T.K. Mayeda, A. Bischoff, Unusual equilibrated carbonaceous chondrites and CO3 meteorites from the Sahara, in Lunar and Planetary Science Conference Abstracts, vol. 27 (1996), p. 1395
D. Weber, L. Schultz, H.W. Weber, R.N. Clayton, T.K. Mayeda, A. Bischoff, Hammadah AL Hamra 119 - a new, unbrecciated Saharan Rumuruti chondrite, in Lunar and Planetary Science Conference Abstracts, vol. 28 (1997), p. 1511
R.C. Weber, P.Y. Lin, E.J. Garnero, Q. Williams, P. Lognonné, Seismic detection of the lunar core. Science 331(6015), 309–312 (2011). https://doi.org/10.1126/science.1199375
M.K. Weisberg, M. Prinz, H. Kojima, K. Yanai, R.N. Clayton, T.K. Mayeda, The Carlisle Lakes-type chondrites: a new grouplet with high \(\varDelta \)17O and evidence for nebular oxidation. Geochim. Cosmochim. Acta 55(9), 2657–2669 (1991). https://doi.org/10.1016/0016-7037(91)90380-N
M.K. Weisberg, M. Prinz, R.N. Clayton, T.K. Mayeda, The CR (Renazzo-type) carbonaceous chondrite group and its implications. Geochim. Cosmochim. Acta 57(7), 1567–1586 (1993). https://doi.org/10.1016/0016-7037(93)90013-M
M. Weisberg, M. Prinz, R. Clayton, T. Mayeda, M. Grady, C. Pillinger, The CR chondrite clan, in Proceedings of the NIPR Symposium on Antarctic Meteorites, vol. 8 (1995), pp. 11–32
M.K. Weisberg, M. Prinz, R.N. Clayton, T.K. Mayeda, M.M. Grady, I. Franchi, C.T. Pillinger, G.W. Kallemeyn, The K (Kakangari) chondrite grouplet. Geochim. Cosmochim. Acta 60(21), 4253–4263 (1996). https://doi.org/10.1016/S0016-7037(96)00233-5
M.K. Weisberg, M. Prinz, R.N. Clayton, T.K. Mayeda, CV3 chondrites: three subgroups, not two. Meteorit. Planet. Sci. 32, A138–A139 (1997)
G.W. Wetherill, Radiometric chronology of early Solar-System. Annu. Rev. Nucl. Sci. 25(1), 283–328 (1975). https://doi.org/10.1146/annurev.ns.25.120175.001435
U. Wiechert, A.N. Halliday, D.C. Lee, G.A. Snyder, L.A. Taylor, D. Rumble, Oxygen isotopes and the Moon-forming giant impact. Science 294(5541), 345–348 (2001). https://doi.org/10.1126/science.1063037
S.A. Wilde, J.W. Valley, W.H. Peck, C.M. Graham, Evidence from detrital zircons for the existence of continental crust and oceans on the Earth 4.4 Gyr ago. Nature 409(6817), 175–178 (2001). https://doi.org/10.1038/35051550
M. Willbold, T. Elliott, S. Moorbath, The tungsten isotopic composition of the Earth’s mantle before the terminal bombardment. Nature 477(7363), 195–198 (2011). https://doi.org/10.1038/nature10399
M. Willbold, S.J. Mojzsis, H.W. Chen, T. Elliott, Tungsten isotope composition of the Acasta Gneiss Complex. Earth Planet. Sci. Lett. 419, 168–177 (2015). https://doi.org/10.1016/j.epsl.2015.02.040
J.G. Williams, A.S. Konopliv, D.H. Boggs, R.S. Park, D.N. Yuan, F.G. Lemoine, S. Goossens, E. Mazarico, F. Nimmo, R.C. Weber, S.W. Asmar, H.J. Melosh, G.A. Neumann, R.J. Phillips, D.E. Smith, S.C. Solomon, M.M. Watkins, M.A. Wieczorek, J.C. Andrews-Hanna, J.W. Head, W.S. Kiefer, I. Matsuyama, P.J. McGovern, G.J. Taylor, M.T. Zuber, Lunar interior properties from the GRAIL mission. J. Geophys. Res., Planets 119(7), 1546–1578 (2014). https://doi.org/10.1002/2013JE004559
J. Wimpenny, N. Marks, K. Knight, J.M. Rolison, L. Borg, G. Eppich, J. Badro, F.J. Ryerson, M. Sanborn, M.H. Huyskens, Y. Qz, Experimental determination of Zn isotope fractionation during evaporative loss at extreme temperatures. Geochim. Cosmochim. Acta 259, 391–411 (2019). https://doi.org/10.1016/j.gca.2019.06.016
J. Wisdom, Z. Tian, Early evolution of the Earth-Moon system with a fast-spinning Earth. Icarus 256, 138–146 (2015). https://doi.org/10.1016/j.icarus.2015.02.025
A. Yamakawa, K. Yamashita, A. Makishima, E. Nakamura, Chromium isotope systematics of achondrites: chronology and isotopic heterogeneity of the inner solar system bodies. Astrophys. J. 720(1), 150–154 (2010). https://doi.org/10.1088/0004-637X/720/1/150
K. Yamashita, T. Ueda, N. Najamura, N. Kita, L.M. Heaman, Chromium isotopic study of Mesosiderite and Ureilite: evidence for \(\epsilon \)54Cr deficit in differentiated meteorites, in NIPR Symposium on Antarctic Meteorites, vol. 29 (2005), pp. 100–101
K. Yamashita, S. Maruyama, A. Yamakawa, E. Nakamura, 53Mn-53Cr chronometry of CB chondrite: evidence for uniform distribution of 53Mn in the early solar system. Astrophys. J. 723(1), 20–24 (2010). https://doi.org/10.1088/0004-637X/723/1/20
Q. Yin, S.B. Jacobsen, K. Yamashita, Diverse supernova sources of pre-solar material inferred from molybdenum isotopes in meteorites. Nature 415(6874), 881–883 (2002). https://doi.org/10.1038/415881a
R. Yokochi, B. Marty, Geochemical constraints on mantle dynamics in the Hadean. Earth Planet. Sci. Lett. 238(1–2), 17–30 (2005). https://doi.org/10.1016/j.epsl.2005.07.020
T. Yoshino, Y. Makino, T. Suzuki, T. Hirata, Grain boundary diffusion of W in lower mantle phase with implications for isotopic heterogeneity in oceanic island basalts by core-mantle interactions. Earth Planet. Sci. Lett. 530, 115,887 (2020). https://doi.org/10.1016/j.epsl.2019.115887
E.D. Young, H. Tang, Isotopic fractionation of moderately volatile elements during Moon formation, in Lunar and Planetary Science Conference Abstracts, vol. 50 (2019), p. 1941
E.D. Young, I.E. Kohl, P.H. Warren, D.C. Rubie, S.A. Jacobson, A. Morbidelli, Oxygen isotopic evidence for vigorous mixing during the Moon-forming giant impact. Science 351(6272), 493–496 (2016). https://doi.org/10.1126/science.aad0525
J. Zhang, N. Dauphas, A.M. Davis, A. Pourmand, A new method for MC-ICPMS measurement of titanium isotopic composition: identification of correlated isotope anomalies in meteorites. J. Anal. At. Spectrom. 26(11), 2197–2205 (2011). https://doi.org/10.1039/c1ja10181a
J. Zhang, N. Dauphas, A.M. Davis, I. Leya, A. Fedkin, The proto-Earth as a significant source of lunar material. Nat. Geosci. 5(4), 251–255 (2012). https://doi.org/10.1038/ngeo1429
M.E. Zolensky, D.W. Mittlefehldt, M.E. Lipschutz, X. Xiao, R.N. Clayton, T.K. Mayeda, R.A. Barrett, M.M. Grady, The composition and mineralogy of EET 83334. Meteoritics 24, 345 (1989)
M.E. Zolensky, D.W. Mittlefehldt, M.E. Lipschutz, M.S. Wang, R.N. Clayton, T.K. Mayeda, M.M. Grady, C. Pillinger, D. Barber, CM chondrites exhibit the complete petrologic range from type 2 to 1. Geochim. Cosmochim. Acta 61(23), 5099–5115 (1997). https://doi.org/10.1016/S0016-7037(97)00357-8
Acknowledgements
This paper was instigated at the International Space Science Institute (ISSI) workshop ‘Reading Terrestrial Planet Evolution in Isotopes and Element Measurements’ and the authors would like to thank ISSI and Europlanet for their support. We would also like to thank Paolo Sossi and an anonymous reviewer for comments that helped improve the clarity and completeness of the manuscript, and Helmut Lammer for editorial handling. We thank Jessica Barnes for providing their Cl isotope database. SJL acknowledges funding from NSF (awards EAR-1947614 and EAR-1725349) and the Division of Geological and Planetary Sciences at the California Institute of Technology. KRB acknowledges funding from NASA Emerging Worlds grants 80NSSC18K0496 and NNX16AN07G, NASA SSERVI grant NNA14AB07A, and support from the Department of Earth and Planetary Sciences, Rutgers University. RP acknowledges support from Washington University. MB received funding from the European Research Council (ERC Grant agreement No. 682778 - ISOREE).
Author information
Authors and Affiliations
Corresponding author
Additional information
Publisher’s Note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Reading Terrestrial Planet Evolution in Isotopes and Element Measurements
Edited by Helmut Lammer, Bernard Marty, Aubrey L. Zerkle, Michel Blanc, Hugh O’Neill and Thorsten Kleine
Appendix
Appendix
1.1 A.1 Data Sources for Figs. 5 and 6
Data for Figs. 5 and 6 were taken from a compilation by Dauphas (2017) with the exception that the lunar value for \(\epsilon\)54Cr was taken from Mougel et al. (2018). Below, we give the original data sources for this compilation.
1.1.1 A.1.1 \(\Delta\)17O
\(\Delta\)17O data was compiled by Dauphas (2017) with the aid of MetBase (Meteorite Information Database, http://www.metbase.org/). \(\Delta\)17O data were taken from Bischoff et al. (1991, 1993, 1998), Bischoff (1994), Bridges et al. (1997, 1999), Brearley et al. (1989), Burkhardt et al. (2017), Buchanan et al. (1993), Clayton and Mayeda (1978, 1981, 1984, 1985, 1989, 1990, 1996), Clayton et al. (1976, 1977, 1983, 1984a,b, 1991, 1997a,b), Connolly et al. (2007), Franchi et al. (1992, 1999), Grossman and Zipfel (2001), Grossman et al. (1987), Grossman (1999), Grady et al. (1987), Gooding et al. (1983), Goodrich et al. (1987), Halbout et al. (1984, 1986), Ivanov et al. (1987), Jabeen et al. (1998), Jackel et al. (1996), Kallemeyn et al. (1996), Keller et al. (1994), McCoy et al. (1995, 1996, 1997), Mayeda and Clayton (1980, 1983, 1989a,b), Mayeda et al. (1987, 1995), Moroz et al. (1988), Nehru et al. (1996), Olsen et al. (1987, 1994), Onuma et al. (1978, 1983), Petaev et al. (1988), Prinz et al. (1991), Pun et al. (1991), Romanek et al. (1998), Rowe et al. (1994), Russell et al. (1998, 2005), Ruzicka et al. (1995), Recca et al. (1986), Sears et al. (1990), Simon et al. (1995), Schulze et al. (1994), Stepniewski et al. (1998), Weber et al. (1996, 1997), Weisberg et al. (1991, 1993, 1995, 1996, 1997), Zolensky et al. (1989, 1997); and Young et al. (2016).
1.1.2 A.1.2 \(\epsilon\)50Ti
\(\epsilon\)50Ti data were taken from Zhang et al. (2011, 2012), Trinquier et al. (2009); and Burkhardt et al. (2017).
1.1.3 A.1.3 \(\epsilon\)54Cr
\(\epsilon\)54Cr data were taken from Trinquier et al. (2007), Qin et al. (2010a,b), Shukolyukov and Lugmair (2006a,b), Shukolyukov et al. (2009), Schiller et al. (2014), Yamashita et al. (2005, 2010), Yamakawa et al. (2010), Larsen et al. (2011), Göpel and Birck (2010), Burkhardt et al. (2017); and Mougel et al. (2018).
1.2 A.2 Details of Mixing Model
In Sect. 6 we present the results of a mixing model to investigate the requirements for mixing during and after the Moon-forming giant impact imposed by the isotopic similarity between the Earth and Moon. Here we provide the details of that model.
We divide the post-impact body into two regions: the Moon-forming region and an isolate region that does not communicate with the Moon forming region during the period of Moon formation. The mass of these two regions are \(M_{1}\) and \(M_{2}\) respectively, where 1 denotes the Moon-forming region and 2 the isolated region (Fig. 8). The masses of the two regions are such that
where \(M_{\mathrm{Moon}}\) and \(M_{\mathrm{Earth}}\) are the mass of the present-day Moon and Earth respectively.
The two regions are made up of a different mass fraction of impactor material, \(f_{\mathrm{imp}}^{i}\), and so have different average \(\Delta\)17O isotopic compositions, \(c_{i}\). Note that both these regions can be internally heterogeneous and the only requirement is that the Moon inherits the average composition of the Moon-forming region. For simplicity, we assume that the majority of Earth mixes after the impact and that the present-day observable mantle is a mixture of the isolated region and the fraction of the Moon-forming region that was not incorporated into the Moon such that
where \(c_{\mathrm{Earth}}\) is the composition of the present-day Earth’s mantle which is zero by definition. The composition of each region is related to the composition of the target and impactor by
where \(c_{\mathrm{imp}}\) and \(c_{\mathrm{tar}}\) are the \(\Delta\)17O isotopic composition of the impactor and target respectively.
We can determine an expression for the mass fraction of the post-impact structure that must be mixed in to the Moon-forming region (\(F_{\mathrm{mix}}=M_{1}/(M_{1}+M_{2})=M_{1}/(M_{ \mathrm{Earth}}+M_{\mathrm{Moon}})\)) given a present-day difference in \(\Delta\)17O between the Moon and Earth (\(\varDelta c_{\mathrm{M-E}}=c_{1}\) by definition), a specified \(\Delta\)17O offset between the impactor and target (\(\varDelta c_{\mathrm{imp-tar}}=c_{\mathrm{imp}}-c_{\mathrm{tar}}\)), and a difference in the mass fraction of impactor in the two regions (\(\varDelta f_{\mathrm{imp}} = f_{\mathrm{imp}}^{1} - f_{\mathrm{imp}}^{2}\)). By substituting for \(M_{2}\) in equation (2) using equation (1) we can find an expression for \(M_{1}\) as a function of the composition of the two regions:
Independently we can re-express equation 2 for the isolated region (\(i=2\)) to give an expression for \(c_{2}\) in terms of the composition of the impactor and target:
Similarly, rearranging equation (2) for the Moon-forming region (\(i=1\)) we obtain an expression for \(c_{\mathrm{imp}}\):
Substituting for \(c_{\mathrm{imp}}\) in equation (5) using equation (6) we obtain
Substituting for \(c_{2}\) in equation (4) using equation (7) and rearranging we find that
or alternatively:
The expression given in equation (9) is significant as it relates the degree of post-impact mixing that is required to explain the Earth-Moon isotopic similarity for a given degree of intra-impact mixing and compositional difference between impactor and target. We can therefore use it to understand the trade offs between mixing during and after the impact (Sect. 6).
Rights and permissions
About this article
Cite this article
Lock, S.J., Bermingham, K.R., Parai, R. et al. Geochemical Constraints on the Origin of the Moon and Preservation of Ancient Terrestrial Heterogeneities. Space Sci Rev 216, 109 (2020). https://doi.org/10.1007/s11214-020-00729-z
Received:
Accepted:
Published:
DOI: https://doi.org/10.1007/s11214-020-00729-z