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Mineral dissolution and reprecipitation mediated by an amorphous phase

Mineral dissolution and reprecipitation mediated by an amorphous phase

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_617d2a465c764081bb96821e9691bf65

Mineral dissolution and reprecipitation mediated by an amorphous phase

About this item

Full title

Mineral dissolution and reprecipitation mediated by an amorphous phase

Publisher

London: Nature Publishing Group UK

Journal title

Nature communications, 2018-04, Vol.9 (1), p.1637-9, Article 1637

Language

English

Formats

Publication information

Publisher

London: Nature Publishing Group UK

More information

Scope and Contents

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...

Alternative Titles

Full title

Mineral dissolution and reprecipitation mediated by an amorphous phase

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_doaj_primary_oai_doaj_org_article_617d2a465c764081bb96821e9691bf65

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_617d2a465c764081bb96821e9691bf65

Other Identifiers

ISSN

2041-1723

E-ISSN

2041-1723

DOI

10.1038/s41467-018-03944-z

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