ESTIMATION OF FORMATION CONDITIONS OF MINERAL MEGASYSTEMS FROM THERMODYNAMIC MODELING
| dc.contributor.author | Chudnenko K.V. | |
| dc.contributor.author | Avchenko O.V. | |
| dc.contributor.author | Aleksandrov I.A. | |
| dc.date.accessioned | 2026-04-25T09:32:57Z | |
| dc.date.issued | 2007 | |
| dc.description.abstract | The temperature and pressure of the formation of mineral assemblages and composition of fluid are currently estimated largely with the method of phase correspondence [1, 2]. This method consists in calculation (on a thermodynamic or experimental basis) of a certain stoichiometric mineral reaction, end member relationship, or a complex of certain reactions that determine the PT parameters and fugacity of volatile components. | |
| dc.identifier | https://elibrary.ru/item.asp?id=15292224 | |
| dc.identifier.citation | Doklady Earth Sciences, 2007, 416, 1, 1132-1136 | |
| dc.identifier.doi | 10.1134/S1028334X07070343 | |
| dc.identifier.issn | 1028-334X | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/52621 | |
| dc.title | ESTIMATION OF FORMATION CONDITIONS OF MINERAL MEGASYSTEMS FROM THERMODYNAMIC MODELING | |
| dc.type | Статья |
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