Metamorphic fluids in orogenic settings

Katy A. Evans, Andrew G. Tomkins

Research output: Contribution to journalArticleResearchpeer-review

1 Citation (Scopus)


etamorphic reactions within the Earth's crust produce fluids of variable composition that play a major role in the evolution of continents. Metamorphic fluids facilitate reactions that alter crustal rheology, reduce melting temperature, cycle elements between geological reservoirs and form ore deposits. These fluids are relatively inaccessible, other than by study of fluid inclusions, so most studies rely on a combination of indirect evidence and predictive thermodynamic models to determine the characteristics and roles of the fluids. In this article, the origins, compositions, controlling phase equilibria, and roles of metamorphic fluids are reviewed, followed by a discussion of selected areas of current and future research.

Original languageEnglish
Pages (from-to)381-387
Number of pages7
Issue number6
Publication statusPublished - Dec 2020


  • Crust
  • Fluid
  • Metamorphic
  • Mineralisation
  • Orogenic
  • Thermodynamics

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