Reference Type | Journal (article/letter/editorial) |
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Title | Structural similarities of some secondary lead minerals |
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Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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Authors | Fanfani, L. | Author |
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Zanazzi, P. F. | Author |
Year | 1967 (December) | Volume | 36 |
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Issue | 280 |
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Publisher | Mineralogical Society |
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Download URL | https://rruff.info/doclib/MinMag/Volume_36/36-280-522.pdf+ |
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DOI | doi:10.1180/minmag.1967.036.280.06Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 6114 | Long-form Identifier | mindat:1:5:6114:2 |
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GUID | 0 |
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Full Reference | Fanfani, L., Zanazzi, P. F. (1967) Structural similarities of some secondary lead minerals. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (280) 522-529 doi:10.1180/minmag.1967.036.280.06 |
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Plain Text | Fanfani, L., Zanazzi, P. F. (1967) Structural similarities of some secondary lead minerals. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (280) 522-529 doi:10.1180/minmag.1967.036.280.06 |
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In | (1966) Mineralogical Magazine Vol. 36 (280) Mineralogical Society |
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Abstract/Notes | SummarySome structural analogies found in tsumebite, vauquelinite, fornacite, and brackebuschite make it possible to place these secondary lead minerals in the same series with general formula Pb2MeII(Z)(XO4)(YO4), where MeII is a bivalent cation as Cu2+ or Mn2+, Z is the hydroxyl group or the water molecule, X is S, Cr, or V, and Y is P, As, or V. Some crystallochemical considerations are developed in order to explain how the replacement of these elements affects the crystal structure in these substances. |
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