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Postdiagenetic Changes in Kerogen Properties and Type by Bacterial Oxidation and Dehydrogenation
A significant part of organic carbon found on the earth is deposited as fossil organic matter in the lithosphere. The most important reservoir of carbon is shale rocks enriched with organic matter in the form of kerogen created during diagenesis. The purpose of this study was to analyze whether the...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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MDPI
2022
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9030554/ https://www.ncbi.nlm.nih.gov/pubmed/35458606 http://dx.doi.org/10.3390/molecules27082408 |