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