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Ostwald, Joseph, England, Brian M. (1979) The relationship between euhedral and framboidal pyrite in base-metal sulphide ores. Mineralogical Magazine, 43 (326) 297-300 doi:10.1180/minmag.1979.043.326.13

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Reference TypeJournal (article/letter/editorial)
TitleThe relationship between euhedral and framboidal pyrite in base-metal sulphide ores
JournalMineralogical MagazineISSN0026-461X
AuthorsOstwald, JosephAuthor
England, Brian M.Author
Year1979 (June)Volume43
Issue326
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_43/43-326-297.pdf+
DOIdoi:10.1180/minmag.1979.043.326.13Search in ResearchGate
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Mindat Ref. ID3024Long-form Identifiermindat:1:5:3024:7
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Full ReferenceOstwald, Joseph, England, Brian M. (1979) The relationship between euhedral and framboidal pyrite in base-metal sulphide ores. Mineralogical Magazine, 43 (326) 297-300 doi:10.1180/minmag.1979.043.326.13
Plain TextOstwald, Joseph, England, Brian M. (1979) The relationship between euhedral and framboidal pyrite in base-metal sulphide ores. Mineralogical Magazine, 43 (326) 297-300 doi:10.1180/minmag.1979.043.326.13
In(1979, June) Mineralogical Magazine Vol. 43 (326) Mineralogical Society
Abstract/NotesSummarySpecimens of layered baryte containing a range of pyrite forms, including framboids, framboidal aggregates, spherulites, polyhedra, and zoned euhedral crystals from Kempfield, New South Wales, Australia, have been examined by mineragraphy, X-ray diffraction (XRD), X-ray fluorescence (XRF), and electron-probe microanalysis (EPMA). These investigations showed that the pyrite occurred in two forms—an arsenical variety containing approximately 5% arsenic in solid solution within the pyrite and a non-arsenical variety. EPMA studies indicate that the framboids and the cores of the zoned euhedral crystals have similar levels of arsenic and a genetic relationship is deduced to exist between these forms.

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