FRACTAL FEATURES AND MORPHOLOGICAL DIFFERENCES BETWEEN PERIODIC INFILTRATION AND DIFFUSION METASOMATIC ZONATION

dc.contributor.author	Rusinov V.L.
dc.contributor.author	Zhukov V.V.
dc.contributor.author	Bityutskaya L.A.
dc.contributor.author	Bogatikov E.V.
dc.date.accessioned	2024-10-23T07:16:02Z
dc.date.available	2024-10-23T07:16:02Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13512609
dc.identifier.citation	Doklady Earth Sciences, 2006, 409, 5, 769-773
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46167
dc.description.abstract	According to the theory based on the principle of local chemical equilibrium in the solution–rock system, the metasomatic zonation is divided into the infiltration and diffusion dynamic types. The formation of zonality during highly nonequilibrium metasomatic processes can produce rhythmic-banded structures that complicate the vectorial (unidirectional) zonation. To interpret such structures, the theory of zonation has been supplemented by a dynamic–kinetic model of the periodic (rhythmic-banded) metasomatic zonation.
dc.title	FRACTAL FEATURES AND MORPHOLOGICAL DIFFERENCES BETWEEN PERIODIC INFILTRATION AND DIFFUSION METASOMATIC ZONATION
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06050217

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