The DOI matches its Crossref record; 4 of the 4 references it cites were found in a registry or an index.
Identification of the giant impactor Theia in lunar rocks
Abstract
An analysis of motes of the Moon maker: How did the Moon form? According to the prevailing hypothesis, a Mars-sized body known as Theia smashed into Earth. Herwartz et al. analyzed fresh basalt samples from three Apollo landing sites and compared them with several samples of Earth's mantle. The oxygen isotope values measured in these lunar rocks differ significantly from the terrestrial material, supporting the giant-impact hypothesis. Science , this issue p. 1146
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Cites
Origin of the Moon in a giant impact near the end of the Earth's formation
Canup, R. M., & Asphaug, E. (2001) · Nature · doi:10.1038/35089010 · Cited by 1,094
A Component of Primitive Nuclear Composition in Carbonaceous Meteorites
Clayton, R. N., Grossman, L., & Mayeda, T. K. (1973) · Science · doi:10.1126/science.182.4111.485 · Cited by 798
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
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
Cited by
Melting and mixing states of the Earth’s mantle after the Moon-forming impact
Nakajima, M., & Stevenson, D. J. (2015) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2015.06.023 · Cited by 215
Metadata
- Authors
- Herwartz, D., Pack, A., Friedrichs, B., & Bischoff, A.
- Venue
- Science
- Published
- 2014-06-06
- Volume
- 344
- Issue
- 6188
- Pages
- 1146-1150
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2057676626
- Cited by
- 199
- References
- 4
- FWCI
- 14.19
- Type
- journal article
- Language
- en
- Open access
- closed
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