ESTIMATION OF FORMATION CONDITIONS OF MINERAL MEGASYSTEMS FROM THERMODYNAMIC MODELING

dc.contributor.authorChudnenko K.V.
dc.contributor.authorAvchenko O.V.
dc.contributor.authorAleksandrov I.A.
dc.date.accessioned2026-04-25T09:32:57Z
dc.date.issued2007
dc.description.abstractThe 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.identifierhttps://elibrary.ru/item.asp?id=15292224
dc.identifier.citationDoklady Earth Sciences, 2007, 416, 1, 1132-1136
dc.identifier.doi10.1134/S1028334X07070343
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/52621
dc.titleESTIMATION OF FORMATION CONDITIONS OF MINERAL MEGASYSTEMS FROM THERMODYNAMIC MODELING
dc.typeСтатья

Файлы

Оригинальный пакет

Показано 1 - 1 из 1
Загрузка...
Изображение-миниатюра
Имя:
Chud_07.pdf
Размер:
166.4 KB
Формат:
Adobe Portable Document Format

Коллекции