Trace element catalyses mineral replacement reactions and facilitates ore formation

Reaction-induced porosity is a key factor enabling protracted fluid-rock interactions in the Earth’s crust, promoting large-scale mineralogical changes during diagenesis, metamorphism, and ore formation. Here, we show experimentally that the presence of trace amounts of dissolved cerium increases th...

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Detalles Bibliográficos
Autores principales: Xing, Yanlu, Brugger, Joël, Etschmann, Barbara, Tomkins, Andrew G., Frierdich, Andrew J., Fang, Xiya
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7925538/
https://www.ncbi.nlm.nih.gov/pubmed/33654089
http://dx.doi.org/10.1038/s41467-021-21684-5

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7925538/
https://www.ncbi.nlm.nih.gov/pubmed/33654089
http://dx.doi.org/10.1038/s41467-021-21684-5

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