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Carbon-bearing iron phases and the carbon isotope composition of the deep Earth
The carbon budget and dynamics of the Earth’s interior, including the core, are currently very poorly understood. Diamond-bearing, mantle-derived rocks show a very well defined peak at δ(13)C ≈ −5 ± 3‰ with a very broad distribution to lower values (∼−40‰). The processes that have produced the wide...
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| Gepubliceerd in: | Proc Natl Acad Sci U S A |
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| Hoofdauteurs: | , |
| Formaat: | Artigo |
| Taal: | Inglês |
| Gepubliceerd in: |
National Academy of Sciences
2015
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| Onderwerpen: | |
| Online toegang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4291649/ https://ncbi.nlm.nih.gov/pubmed/25512520 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1401782112 |
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