Mineral paragenesis on Mars: The roles of reactive surface area and diffusion

Geochemical models of secondary mineral precipitation on Mars generally assume semiopen systems (open to the atmosphere but closed at the water‐sediment interface) and equilibrium conditions. However, in natural multicomponent systems, the reactive surface area of primary minerals controls the disso...

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Detalles Bibliográficos
Autores principales: Fairén, Alberto G., Gil‐Lozano, Carolina, Uceda, Esther R., Losa‐Adams, Elisabeth, Davila, Alfonso F., Gago‐Duport, Luis
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2017
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5656915/
https://www.ncbi.nlm.nih.gov/pubmed/29104844
http://dx.doi.org/10.1002/2016JE005229

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5656915/
https://www.ncbi.nlm.nih.gov/pubmed/29104844
http://dx.doi.org/10.1002/2016JE005229

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