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Oldhamite: a new link in upper mantle for C–O–S–Ca cycles and an indicator for planetary habitability
In the solar system, oldhamite (CaS) is generally considered to be formed by the condensation of solar nebula gas. Enstatite chondrites, one of the most important repositories of oldhamite, are believed to be representative of the material that formed Earth. Thus, the formation mechanism and the evo...
| Autores principales: | , , , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Oxford University Press
2023
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10476894/ https://www.ncbi.nlm.nih.gov/pubmed/37671325 http://dx.doi.org/10.1093/nsr/nwad159 |