Volume self-diffusion of oxygen in biotite, muscovite, and phlogopite micas

Details Volume self-diffusion of oxygen in biotite, muscovite, and phlogopite micas Volume self-diffusion of oxygen in biotite, muscovite, and phlogopite micas

May 1991

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991gecoa..55.1319f&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 55, Issue 5, pp.1319-1330

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Scientific paper

The kinetics of oxygen self-diffusion have been measured in natural samples of biotite, muscovite, and phlogopite micas under hydrothermal conditions using both bulk exchange and profiling analyses. All experiments were run at 1000 bars (100 MPa) water pressure except those designed to measure water pressure dependence, which ranged from 200 to 2000 bars. The Arrhenius relations obtained for layer-parallel diffusive transport in the three micas by bulk exchange experiments, fit to an infinite cylinder model, are

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