Steady diffusion model for olivine-plagioclase corona growth-Reference-Cited by-同舟云学术

Steady diffusion model for olivine-plagioclase corona growth

Published:1983-02 Issue:2 Volume:47 Page:283-294
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Nishiyama Tadao

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference35 articles.

1. Metazomatic zones in metamorphic rocks;Brady;Geochim. Cosmochim. Acta,1977

2. Chain Silicates;Deer,1963

3. Corona structures formed by nearisochemical reaction between olivine and plagioclase in a metamorphosed dolerite;England;Mineral. Mag.,1974

4. Coronites from the Fongen gabbro complex, Trondheim Region. Norway: role of water in the olivine-plagioclase reaction;Esbensen;N. Jb. Mineral. Abh.,1978

5. Non-equilibrium thermodynamics as a model for diffusion controlled metamorphic processes;Fisher;Amer. J. Sci.,1973

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