| Reference Type | Journal (article/letter/editorial) |
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| Title | Marshite–miersile solid solution and iodargyrite from Broken Hill, New South Wales, Australia |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Millsteed, P. W. | Author |
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| Year | 1998 (August) | Volume | 62 |
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| Issue | 4 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_62/62-4-471.pdf+ |
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| DOI | doi:10.1180/002646198547846Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 296 | Long-form Identifier | mindat:1:5:296:9 |
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| GUID | 0 |
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| Full Reference | Millsteed, P. W. (1998) Marshite–miersile solid solution and iodargyrite from Broken Hill, New South Wales, Australia. Mineralogical Magazine, 62 (4) 471-475 doi:10.1180/002646198547846 |
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| Plain Text | Millsteed, P. W. (1998) Marshite–miersile solid solution and iodargyrite from Broken Hill, New South Wales, Australia. Mineralogical Magazine, 62 (4) 471-475 doi:10.1180/002646198547846 |
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| Abstract/Notes | Abstract
Microprobe analysis of marshite and miersite from Broken Hill, Australia, demonstrate extensive solid solution between the end-members CuI and AgI, indicating the possibility of a complete solid-solution series. Unit-cell parameters increase from 6.054 Å for marshite to 6.504 Å for miersite, closely following Vegard's Law. The Cu content of iodargyrite is generally below the limit of detection, but one zoned crystal contained 0.28 wt.% Cu. Crystallization of either miersite or iodargyrite at Broken Hill appears to be dependent upon the local availability and ratio of copper, silver and iodine ions. |
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