TRANSITION TO LOCAL EQUILIBRIUM IN THE DEVELOPMENT OF A DIFFUSIONAL BIMETASOMATIC ZONE

dc.contributor.author	Balashov V.N.
dc.contributor.author	Lebedeva M.I.
dc.date.accessioned	2020-10-08T10:25:17Z
dc.date.available	2020-10-08T10:25:17Z
dc.date.issued	1989
dc.identifier	https://elibrary.ru/item.asp?id=31092077
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1989, , 4, 183-187
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/17785
dc.description.abstract	One promising area of theoretical research on metasomatism is the development of a macrokinetic model based on reversible reactions. The present paper describes a numerical investigation of a model of bimetasomatism in isothermal systems with solid two-component mineral phases of constant composition. The interstitial phase transporting the components is a dilute hydrothermal solution. The pressure on the minerals is constant and equal to the pressure of the interstitial solution. Under these conditions the chemical potential of water is governed almost exclusively by P and T.
dc.title	TRANSITION TO LOCAL EQUILIBRIUM IN THE DEVELOPMENT OF A DIFFUSIONAL BIMETASOMATIC ZONE
dc.type	Статья

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