Cargando…
Carbonate formation in salt dome cap rocks by microbial anaerobic oxidation of methane
Major hydrocarbon accumulations occur in traps associated with salt domes. Whereas some of these hydrocarbons remain to be extracted for economic use, significant amounts have degraded in the subsurface, yielding mineral precipitates as byproducts. Salt domes of the Gulf of Mexico Basin typically ex...
Autores principales: | Caesar, K. H., Kyle, J. R., Lyons, T. W., Tripati, A., Loyd, S. J. |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2019
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6379371/ https://www.ncbi.nlm.nih.gov/pubmed/30778057 http://dx.doi.org/10.1038/s41467-019-08687-z |
Ejemplares similares
-
Methane seep carbonates yield clumped isotope signatures out of equilibrium with formation temperatures
por: Loyd, S. J., et al.
Publicado: (2016) -
Anaerobic oxidation of methane: an “active” microbial process
por: Cui, Mengmeng, et al.
Publicado: (2015) -
Thermal influences on spontaneous rock dome exfoliation
por: Collins, Brian D., et al.
Publicado: (2018) -
Rates and Microbial Players of Iron-Driven Anaerobic Oxidation of Methane in Methanic Marine Sediments
por: Aromokeye, David A., et al.
Publicado: (2020) -
Methane and carbon at equilibrium in source rocks
por: Mango, Frank D
Publicado: (2013)