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Rattray, K. J., Taylor, M. R., Bevan, D. J. M., Pring, A. (1996) Compositional segregation and solid solution in the lead-dominant alunite-type minerals from Broken Hill, N.S.W. Mineralogical Magazine, 60 (402) 779-785 doi:10.1180/minmag.1996.060.402.07

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Reference TypeJournal (article/letter/editorial)
TitleCompositional segregation and solid solution in the lead-dominant alunite-type minerals from Broken Hill, N.S.W.
JournalMineralogical MagazineISSN0026-461X
AuthorsRattray, K. J.Author
Taylor, M. R.Author
Bevan, D. J. M.Author
Pring, A.Author
Year1996 (October)Volume60
Issue402
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_60/60-402-779.pdf+
DOIdoi:10.1180/minmag.1996.060.402.07Search in ResearchGate
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Mindat Ref. ID95Long-form Identifiermindat:1:5:95:0
GUID0
Full ReferenceRattray, K. J., Taylor, M. R., Bevan, D. J. M., Pring, A. (1996) Compositional segregation and solid solution in the lead-dominant alunite-type minerals from Broken Hill, N.S.W. Mineralogical Magazine, 60 (402) 779-785 doi:10.1180/minmag.1996.060.402.07
Plain TextRattray, K. J., Taylor, M. R., Bevan, D. J. M., Pring, A. (1996) Compositional segregation and solid solution in the lead-dominant alunite-type minerals from Broken Hill, N.S.W. Mineralogical Magazine, 60 (402) 779-785 doi:10.1180/minmag.1996.060.402.07
In(1996, October) Mineralogical Magazine Vol. 60 (402) Mineralogical Society
Abstract/NotesAbstractA study of the composition and unit cell data of a suite of lead-rich minerals of the alunite-jarosite group from the oxidized zone of the ore body at Broken Hill, New South Wales, Australia, has revealed almost complete XO4 (X = As, P, S) solid solution in these minerals at this deposit. The species in the group noted are hidalgoite, hinsdalite, beudantite, segnitite and plumbogummite. These minerals at Broken Hill exhibit a number of growth textures, including oscillatory zoning, colloform banding and replacements. Zoning in these minerals is due to the segregation of Al- and Fe-rich members, and compositions indicate a strong coupling of Fe3+ with and Al with


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