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Olivine-norite rock detected by the lunar rover Yutu-2 likely crystallized from the SPA-impact melt pool
Chang’E-4 landed in the South Pole-Aitken (SPA) basin, providing a unique chance to probe the composition of the lunar interior. Its landing site is located on ejecta strips in Von Kármán crater that possibly originate from the neighboring Finsen crater. A surface rock and the lunar regolith at 10 s...
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| Veröffentlicht in: | Natl Sci Rev |
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| Hauptverfasser: | , , , , , , , , , , , , , , , , , , , , |
| Format: | Artigo |
| Sprache: | Inglês |
| Veröffentlicht: |
Oxford University Press
2020
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| Schlagworte: | |
| Online Zugang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC8288882/ https://ncbi.nlm.nih.gov/pubmed/34692112 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1093/nsr/nwz183 |
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