THE FUSION CURVE OF ALBITE REVISITED AND THE COMPRESSIBILITY OF NAALSI3O8 LIQUID WITH PRESSURE

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dc.contributor.author Lange R.A.
dc.date.accessioned 2022-01-02T07:44:06Z
dc.date.available 2022-01-02T07:44:06Z
dc.date.issued 2003
dc.identifier https://www.elibrary.ru/item.asp?id=7600095
dc.identifier.citation American Mineralogist, 2003, 88, 1, 109
dc.identifier.issn 0003-004X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/34100
dc.description.abstract The I bar, thermodynamic properties of crystalline and liquid NaAlSi308 are used to calculate the fusion curve of albite to 10 kbar. The calculated temperatures (± 2sigma) of the melting reaction are 1152 (± 7) degrees C at 3 kbar and 1247 (± 24) degrees Cat 10 kbar. The location of the calculated fusion curve to 10 kbar is in excellent agreement with phase-equilibrium constraints on the maximum and minimum temperatures of the fusion curve at 3 and 15 kbar, respectively. Calculation of the melting reaction at pressures >10 kbar requires that the pressure dependence of the liquid compressibility (K0 = dKT,O/ dP, where KT,O = 1BetaT,0) be known. On the basis of five half-reversal, crystallization experiments in the literature, which collectively provide minimum temperatures of the fusion curve between 12 and 32 kbar, KO (derived from the Birch-Murnaghan relation) is constrained to be greater or more than 10 for liquid NaAlSi308A comparison with other silicate liquids shows that there is a strong, positive correlation between the compressibility at one bar (BetaT,O) and K0. In addition, data on the water-saturated fusion curve of albite are used to quantify the effect of small amounts of H20 (less than or equal to 1 wt%) on lowering the melting temperature of albite (less than or equal to 68 degrees).
dc.subject MINERALOGY
dc.subject PRESSURE
dc.title THE FUSION CURVE OF ALBITE REVISITED AND THE COMPRESSIBILITY OF NAALSI3O8 LIQUID WITH PRESSURE
dc.type Статья


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