THE SYSTEM CO2-N2 AT HIGH PRESSURE AND APPLICATIONS TO FLUID INCLUSIONS

dc.contributor.author	Kooi M.E.
dc.contributor.author	Schouten J.A.
dc.contributor.author	van den Kerkhof A.M.
dc.contributor.author	Istrate G.
dc.contributor.author	Althaus E.
dc.date.accessioned	2020-12-29T10:10:03Z
dc.date.available	2020-12-29T10:10:03Z
dc.date.issued	1998
dc.identifier	https://elibrary.ru/item.asp?id=86573
dc.identifier.citation	Geochimica et Cosmochimica Acta, 1998, , 16, 2837-2843
dc.identifier.issn	0016-7037
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/21654
dc.description.abstract	Postulated fluid-fluid immiscibility of 50-50% CO2-N2 mixtures has been checked by high-pressure experiments (<5 gpa; <400 k) and could be rejected. the implications for interpretation of high-density fluid inclusions (<42 cm3/mole) in eclogite and granulite-facies rocks are discussed: only models based on LG-immiscibility are applicable for molar volume calculations also in the very-high-pressure range. The position of the critical curve for CO2-N2 could be more accurately determined with the help of experimental and fluid inclusion data. The S2-F isopleth and the three-phase (S1S2F) line have been established for 50.6% N2 composition.
dc.title	THE SYSTEM CO2-N2 AT HIGH PRESSURE AND APPLICATIONS TO FLUID INCLUSIONS
dc.type	Статья

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