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French, W. J., Cameron, E. P. (1981) Calculation of the temperature of crystallization of silicates from basaltic melts. Mineralogical Magazine, 44 (333) 19-26 doi:10.1180/minmag.1981.44.333.02

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Reference TypeJournal (article/letter/editorial)
TitleCalculation of the temperature of crystallization of silicates from basaltic melts
JournalMineralogical MagazineISSN0026-461X
AuthorsFrench, W. J.Author
Cameron, E. P.Author
Year1981 (March)Volume44
Issue333
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_44/44-333-19.pdf+
DOIdoi:10.1180/minmag.1981.44.333.02Search in ResearchGate
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Mindat Ref. ID3214Long-form Identifiermindat:1:5:3214:2
GUID0
Full ReferenceFrench, W. J., Cameron, E. P. (1981) Calculation of the temperature of crystallization of silicates from basaltic melts. Mineralogical Magazine, 44 (333) 19-26 doi:10.1180/minmag.1981.44.333.02
Plain TextFrench, W. J., Cameron, E. P. (1981) Calculation of the temperature of crystallization of silicates from basaltic melts. Mineralogical Magazine, 44 (333) 19-26 doi:10.1180/minmag.1981.44.333.02
In(1981, March) Mineralogical Magazine Vol. 44 (333) Mineralogical Society
Abstract/NotesAbstractThis paper discusses the relationship between the chemical composition of basic melts and the temperatures at which olivine, clinopyroxene, and plagioclase begin to crystallize at one atmosphere. Diagrams are given which show the correlation between crystallization temperature and melt composition and which allow some of the temperatures to be estimated. Because the relationship between melt composition and crystallization temperature is virtually linear over short compositional ranges, the data available can be subdivided and examined by linear multivariate statistical techniques. The result is a set of equations which permit the crystallization temperatures to be calculated with an average error of less than 6 °C and a maximum error of 27 °C. These equations have been tested by experimental determination of crystallization temperatures for a range of rocks from the Marquesas Islands.


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