| Reference Type | Journal (article/letter/editorial) |
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| Title | The metavoltine problem: metavoltine from Madeni Zakh and Chuquicamata, and a related artificial compound |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Scordari, F. | Author |
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| Year | 1977 (September) | Volume | 41 |
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| Page(s) | 371-374 | Issue | 319 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_41/41-319-371.pdf+ |
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| DOI | doi:10.1180/minmag.1977.041.319.09Search in ResearchGate |
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| Mindat Ref. ID | 2784 | Long-form Identifier | mindat:1:5:2784:1 |
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| GUID | b27d53c7-f31c-4fd9-8689-24f6c493675f |
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| Full Reference | Scordari, F. (1977) The metavoltine problem: metavoltine from Madeni Zakh and Chuquicamata, and a related artificial compound. Mineralogical Magazine, 41 (319) 371-374 doi:10.1180/minmag.1977.041.319.09 |
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| Plain Text | Scordari, F. (1977) The metavoltine problem: metavoltine from Madeni Zakh and Chuquicamata, and a related artificial compound. Mineralogical Magazine, 41 (319) 371-374 doi:10.1180/minmag.1977.041.319.09 |
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| In | (1977, September) Mineralogical Magazine Vol. 41 (319) Mineralogical Society |
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| Abstract/Notes | SummaryBandy (1938) described as metavoltine? a mineral coming from Chuquicamata (Chile) with chemical composition K2Na6Fe3+(SO4)12(OH)2·20H2O. Owing to some differences between this mineral and that first described by Blaas (1883), doubts persist on the identity of these two compounds. X-ray analyses were performed to clarify the relation between them. An artificial product, closely related to metavoltine as regards lattice and chemical composition, was also studied, and affords a better understanding of the Na and K diadochy already observed in metavoltine. |
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