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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...
Wedi'i Gadw mewn:
| Cyhoeddwyd yn: | Proc Natl Acad Sci U S A |
|---|---|
| Prif Awduron: | , , , , |
| Fformat: | Artigo |
| Iaith: | Inglês |
| Cyhoeddwyd: |
National Academy of Sciences
2015
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| Pynciau: | |
| Mynediad Ar-lein: | 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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