Formation of Large Native Sulfur Deposits Does Not Require Molecular Oxygen

Large native (i.e., elemental) sulfur deposits can be part of caprock assemblages found on top of or in lateral position to salt diapirs and as stratabound mineralization in gypsum and anhydrite lithologies. Native sulfur is formed when hydrocarbons come in contact with sulfate minerals in presence...

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Detalles Bibliográficos
Autores principales: Labrado, Amanda L., Brunner, Benjamin, Bernasconi, Stefano M., Peckmann, Jörn
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Frontiers Media S.A. 2019
Materias:
Microbiology
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6355691/
https://www.ncbi.nlm.nih.gov/pubmed/30740094
http://dx.doi.org/10.3389/fmicb.2019.00024

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6355691/
https://www.ncbi.nlm.nih.gov/pubmed/30740094
http://dx.doi.org/10.3389/fmicb.2019.00024

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