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Gittins, J., Fawcett, J. J., Rucklidge, J. C., Brooks, C. K. (1982) An occurrence of the spinel end-member Mg2TiO4 and related spinel solid solutions. Mineralogical Magazine, 45 (337) 135-137 doi:10.1180/minmag.1982.045.337.15

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Reference TypeJournal (article/letter/editorial)
TitleAn occurrence of the spinel end-member Mg2TiO4 and related spinel solid solutions
JournalMineralogical MagazineISSN0026-461X
AuthorsGittins, J.Author
Fawcett, J. J.Author
Rucklidge, J. C.Author
Brooks, C. K.Author
Year1982Volume45
Issue337
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_45/45-337-135.pdf+
DOIdoi:10.1180/minmag.1982.045.337.15Search in ResearchGate
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Mindat Ref. ID3325Long-form Identifiermindat:1:5:3325:5
GUID0
Full ReferenceGittins, J., Fawcett, J. J., Rucklidge, J. C., Brooks, C. K. (1982) An occurrence of the spinel end-member Mg2TiO4 and related spinel solid solutions. Mineralogical Magazine, 45 (337) 135-137 doi:10.1180/minmag.1982.045.337.15
Plain TextGittins, J., Fawcett, J. J., Rucklidge, J. C., Brooks, C. K. (1982) An occurrence of the spinel end-member Mg2TiO4 and related spinel solid solutions. Mineralogical Magazine, 45 (337) 135-137 doi:10.1180/minmag.1982.045.337.15
In(1982) Mineralogical Magazine Vol. 45 (337) Mineralogical Society
Abstract/NotesAbstractBlack, opaque grains of a spinel whose composition is (Mg2TiO4) 85.8, (MgFe2O4) 0.4 (FeFe2O4) 13.8 (mole %) coexist with a MgAl2O4 spinel and geikielite in a periclase-forsterite marble that has been thermally metamorphosed against an alkalic ultramafic intrusion of Caledonian age in the Kangerdlugssuaq region of East Greenland. The spinel appears to be the closest recorded approach to the end-member Mg2TiO4 among natural rocks, and to be part of a solid-solution series extending across the join Mg2TiO4-MgFe2O4-FeFe2O4, the existence of which has not previously been reported. The composition of the series appears to be controlled by the fO2 that prevails during metamorphism.


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