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Abiotic methane formation during experimental serpentinization of olivine
Fluids circulating through actively serpentinizing systems are often highly enriched in methane (CH(4)). In many cases, the CH(4) in these fluids is thought to derive from abiotic reduction of inorganic carbon, but the conditions under which this process can occur in natural systems remain unclear....
保存先:
| 出版年: | Proc Natl Acad Sci U S A |
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| 第一著者: | |
| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
National Academy of Sciences
2016
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5150391/ https://ncbi.nlm.nih.gov/pubmed/27821742 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1611843113 |
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