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Greigite: a true intermediate on the polysulfide pathway to pyrite
The formation of pyrite (FeS(2)) from iron monosulfide precursors in anoxic sediments has been suggested to proceed via mackinawite (FeS) and greigite (Fe(3)S(4)). Despite decades of research, the mechanisms of pyrite formation are not sufficiently understood because solid and dissolved intermediate...
| Autores principales: | , |
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| Formato: | Texto |
| Lenguaje: | English |
| Publicado: |
BioMed Central
2007
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC1847509/ https://www.ncbi.nlm.nih.gov/pubmed/17376247 http://dx.doi.org/10.1186/1467-4866-8-1 |