Growth of mineral zones by diffusion-controlled reactions: theory and application to mesosiderites.

Details Growth of mineral zones by diffusion-controlled reactions: theory and application to mesosiderites. Growth of mineral zones by diffusion-controlled reactions: theory and application to mesosiderites.

Jan 1998

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1998amjs..298....1r&link_type=abstract

Am. J. Sci., Vol. 298, No. 1, p. 1 - 29

Physics

1

Meteorites: Minerals

Scientific paper

The theory of Fisher (1973, 1977) and Joesten (1977) for the steady-state growth of mineral zones by diffusion-controlled reactions is modified to explicitly and formally account for polymineralic reactants, open-system diffusive fluxes, and diffusion geometry. The modifications are illustrated by applying the theory to olivine coronas in mesosiderite meteorites.

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