A thermodynamic model for Fe–Mg dioctahedral K white micas using data from phase-equilibrium experiments and natural pelitic assemblages

2002/07/09 by Teddy Parra, Olivier Vidal, Phillipe Agard · 8 citations
Materials Science · Earth and Planetary Sciences · #Clay minerals and soil interactions #Geological and Geochemical Analysis #High-pressure geophysics and materials

paper · doi:10.1007/s00410-002-0373-6

Cited by

• Time-strain evolution of shear zones from petrographically constrained Rb–Sr muscovite analysis
• P-T Constraints on the Metamorphic Evolution of the Paleoarchean Kromberg Type-Section, Barberton Greenstone Belt, South Africa
• Microstructural vs compositional preservation and pseudomorphic replacement of muscovite in deformed metapelites from the Longmen Shan (Sichuan, China)
• Structural and chemical resetting processes in white mica and their effect on K-Ar data during low temperature metamorphism
• XMapTools: A MATLAB©-based program for electron microprobe X-ray image processing and geothermobarometry
• Non-conventional pressure estimates by using transmission electron microscopy coupled with energy-dispersive spectroscopy (TEM-EDS): testing on submicrometer white mica from low-grade metapelites
• Modern-style plate subduction preserved in the Palaeoproterozoic West African craton
• Petrological and geochronological constraints on lower crust exhumation during Paleoproterozoic (Eburnean) orogeny, NW Ghana, West African Craton