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Formation of H(2 )and CH(4 )by weathering of olivine at temperatures between 30 and 70°C
Hydrocarbons such as CH(4 )are known to be formed through the Fischer-Tropsch or Sabatier type reactions in hydrothermal systems usually at temperatures above 100°C. Weathering of olivine is sometimes suggested to account for abiotic formation of CH(4 )through its redox lowering and water splitting...
| Autores principales: | , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
BioMed Central
2011
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3157414/ https://www.ncbi.nlm.nih.gov/pubmed/21707970 http://dx.doi.org/10.1186/1467-4866-12-6 |