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Carbonate formation events in ALH 84001 trace the evolution of the Martian atmosphere
Carbonate minerals provide critical information for defining atmosphere–hydrosphere interactions. Carbonate minerals in the Martian meteorite ALH 84001 have been dated to ∼3.9 Ga, and both C and O-triple isotopes can be used to decipher the planet’s climate history. Here we report Δ(17)O, δ(18)O, an...
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| Publicado en: | Proc Natl Acad Sci U S A |
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| Autores principales: | , , , , |
| Formato: | Artigo |
| Lenguaje: | Inglês |
| Publicado: |
National Academy of Sciences
2015
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| Materias: | |
| Acceso en línea: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4299197/ https://ncbi.nlm.nih.gov/pubmed/25535348 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1315615112 |
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