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Nolan, J. (1969) Physical properties of synthetic and natural pyroxenes in the system diopside–hedenbergite–acmite. Mineralogical Magazine, 37 (286) 216-229 doi:10.1180/minmag.1969.037.286.09

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Reference TypeJournal (article/letter/editorial)
TitlePhysical properties of synthetic and natural pyroxenes in the system diopside–hedenbergite–acmite
JournalMineralogical Magazine
AuthorsNolan, J.Author
Year1969 (June)Volume37
Issue286
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_37/37-286-216.pdf+
DOIdoi:10.1180/minmag.1969.037.286.09Search in ResearchGate
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Mindat Ref. ID6258Long-form Identifiermindat:1:5:6258:3
GUID0
Full ReferenceNolan, J. (1969) Physical properties of synthetic and natural pyroxenes in the system diopside–hedenbergite–acmite. Mineralogical Magazine, 37 (286) 216-229 doi:10.1180/minmag.1969.037.286.09
Plain TextNolan, J. (1969) Physical properties of synthetic and natural pyroxenes in the system diopside–hedenbergite–acmite. Mineralogical Magazine, 37 (286) 216-229 doi:10.1180/minmag.1969.037.286.09
In(1969, June) Mineralogical Magazine Vol. 37 (286) Mineralogical Society
Abstract/NotesSummaryUnit cell dimensions and refractive indices have been determined for synthetic pyroxenes in the system CaMgSi2O6-CaFeSi2O6-NaFeSi2O6, which have been crystallized and annealed on the nickel-bunsenite (Ni-NiO) oxygen buffer curve at 700 °C and a total pressure of 2 kb. The data presented confirms the many postulates that a complete solid solution series does exist in the subsolidus region of the ‘ternary’ system. The unit cell dimensions show an almost linear change with composition between the end members. The determined cell parameters for a series of analysed natural alkali pyroxenes have been compared with the data for the synthetic pyroxenes and close agreement was found between both sets of data. The variation of the unit cell dimensions and refractive indices has been examined in relation to the possible ionic substitutions taking place in the pyroxenes.


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