Mineral dissolution and reprecipitation mediated by an amorphous phase
Mineral dissolution and reprecipitation mediated by an amorphous phase
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London: Nature Publishing Group UK
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Language
English
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London: Nature Publishing Group UK
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Contents
Fluid-mediated mineral dissolution and reprecipitation processes are the most common mineral reaction mechanism in the solid Earth and are fundamental for the Earth’s internal dynamics. Element exchange during such mineral reactions is commonly thought to occur via aqueous solutions with the mineral solubility in the coexisting fluid being a rate l...
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Mineral dissolution and reprecipitation mediated by an amorphous phase
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TN_cdi_doaj_primary_oai_doaj_org_article_617d2a465c764081bb96821e9691bf65
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_617d2a465c764081bb96821e9691bf65
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ISSN
2041-1723
E-ISSN
2041-1723
DOI
10.1038/s41467-018-03944-z