STRUCTURAL DISCONTINUITIES IN PLAGIOCLASE AND CONSTRAINTS ON MIXING PROPERTIES OF THE LOW SERIES: A COMPUTATIONAL STUDY

dc.contributor.authorVinograd V.L.
dc.contributor.authorPutnis A.
dc.contributor.authorKroll H.
dc.date.accessioned2021-03-02T00:44:50Z
dc.date.available2021-03-02T00:44:50Z
dc.date.issued2001
dc.description.abstractSubsolidus phase relations in the plagioclase system are investigated using an Ising-type model. The model treats ordering of Al,Si and Na,Ca cations in three dimensions using a version of the cluster variation method. The interactions within the T (Al,Si) and M (Na,Ca) sublattices and the interactions between the T and M sublattices are constrained by the available experimental information on order-disorder transitions in the system. The paper suggests a thermodynamic explanation for the existence of two distinct structural series (high and low) and gives constraints on the thermodynamics of low plagioclases.
dc.identifierhttps://elibrary.ru/item.asp?id=13678066
dc.identifier.citationMineralogical Magazine, 2001, 65, 1, 1-31
dc.identifier.issn0026-461X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/25933
dc.titleSTRUCTURAL DISCONTINUITIES IN PLAGIOCLASE AND CONSTRAINTS ON MIXING PROPERTIES OF THE LOW SERIES: A COMPUTATIONAL STUDY
dc.typeСтатья

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