SOME ENERGETIC PROPERTIES OF MINERAL ASSEMBLAGES

dc.contributor.author	Rakhov E.V.
dc.date.accessioned	2024-10-27T02:28:42Z
dc.date.available	2024-10-27T02:28:42Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13516246
dc.identifier.citation	Doklady Earth Sciences, 2006, 410, 7, 1122-1126
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46242
dc.description.abstract	The energetic aspects of redistribution of chemical bonds of lithospheric material during metamorphism, metasomatism, and hydrothermal activity attract interest in connection with the behavior of chemical elements (concentration and dispersion) in PT-gradient fields and the individual properties of atoms. The main function (isobaric–isothermal potential) used to study the phase relations in heterogeneous systems does not make it possible to analyze the transformation of chemical bonds during the change of mineral assemblages in rocks initiated by variation of intense parameters.
dc.title	SOME ENERGETIC PROPERTIES OF MINERAL ASSEMBLAGES
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06070270

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