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The effect of H2O fluid on relative component mobilities in a bimineralic reaction rim in the system CaO-MgO-SiO2

  • Bastian Joachim
  • , Wilhelm Heinrich
  • , Carmen Hoeschen
  • , Rainer Abart

Publications: Contribution to journalArticlePeer Reviewed

Original languageEnglish
Pages (from-to)61-72
Number of pages12
JournalEuropean Journal of Mineralogy: an international journal of mineralogy, geochemistry and related sciences
Volume31
Issue number1
DOIs
Publication statusPublished - Jan 2019

Funding

We thank J. Lugmeier and C.W. Muller from the TU Munich for their extensive support during NanoSIMS analyses and Gerlinde Habler for recording BSE and SEM images. We also thank two anonymous reviewers for their comments that helped to improve the manuscript. This work was partly funded by the Deutsche Forschungsgemeinschaft in the framework of FOR 741, project HE 2015/9-1, which is gratefully acknowledged.

Austrian Fields of Science 2012

  • 105120 Petrology

Keywords

  • reaction rim
  • bimineralic
  • microstructure
  • wollastonite
  • diopside
  • isotopically labelled
  • NanoSIMS
  • component mobilities
  • hydrous fluid
  • GRAIN-BOUNDARY DIFFUSION
  • ENSTATITE REACTION RIMS
  • THERMODYNAMIC MODEL
  • GROWTH-KINETICS
  • CORONAS
  • RATES
  • OLIVINE
  • MOUNTAINS
  • GRANULITE
  • WATER
  • Isotopically labelled
  • Component mobilities
  • Hydrous fluid
  • Reaction rim
  • Diopside
  • Bimineralic
  • Wollastonite
  • Microstructure

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