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
Reference Type | Journal (article/letter/editorial) | ||
---|---|---|---|
Title | Compositional segregation and solid solution in the lead-dominant alunite-type minerals from Broken Hill, N.S.W. | ||
Journal | Mineralogical Magazine | ISSN | 0026-461X |
Authors | Rattray, K. J. | Author | |
Taylor, M. R. | Author | ||
Bevan, D. J. M. | Author | ||
Pring, A. | Author | ||
Year | 1996 (October) | Volume | 60 |
Page(s) | 779-785 | Issue | 402 |
Publisher | Mineralogical Society | ||
Download URL | https://rruff.info/doclib/MinMag/Volume_60/60-402-779.pdf+ | ||
DOI | doi:10.1180/minmag.1996.060.402.07Search in ResearchGate | ||
Mindat Ref. ID | 95 | Long-form Identifier | mindat:1:5:95:0 |
GUID | 0cbd48f6-21b0-48b8-a9d0-6ab25d4c0ad6 | ||
Full Reference | 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 | ||
Plain Text | 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 | ||
In | (1996, October) Mineralogical Magazine Vol. 60 (402) Mineralogical Society | ||
Abstract/Notes | AbstractA 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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