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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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| Pubblicato in: | Proc Natl Acad Sci U S A |
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| Autori principali: | , , , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
National Academy of Sciences
2015
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| Soggetti: | |
| Accesso online: | 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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