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- W2322553492 abstract "Natural magmatic, metamorphic, and metasomatic processes proceed under conditions of open systems and under the action of diffusion and infiltration streams of matter with different mobility of components. During diffusion metasomatism, the composition of a mineral solid solution changes gradually within each zone, whereas in infiltration metasomatism the mineral composition remains constant within a given zone. In systems in which the acidity and the reduction potential are externally controlled, the acid-base interaction of components furnishes another criterion for distinguishing infiltration from diffusion processes." @default.
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- W2322553492 date "1965-03-01" @default.
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- W2322553492 title "The theory of systems with perfectly mobile components and processes of mineral formation" @default.
- W2322553492 doi "https://doi.org/10.2475/ajs.263.3.193" @default.
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