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Generation of methane in the Earth's mantle: In situ high pressure–temperature measurements of carbonate reduction
We present in situ observations of hydrocarbon formation via carbonate reduction at upper mantle pressures and temperatures. Methane was formed from FeO, CaCO(3)-calcite, and water at pressures between 5 and 11 GPa and temperatures ranging from 500°C to 1,500°C. The results are shown to be consisten...
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| 主要な著者: | , , , , , , |
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| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
National Academy of Sciences
2004
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC521091/ https://ncbi.nlm.nih.gov/pubmed/15381767 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0405930101 |
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