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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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Reference TypeJournal (article/letter/editorial)
TitleStructural similarities of some secondary lead minerals
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsFanfani, L.Author
Zanazzi, P. F.Author
Year1967 (December)Volume36
Issue280
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_36/36-280-522.pdf+
DOIdoi:10.1180/minmag.1967.036.280.06Search in ResearchGate
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Mindat Ref. ID6114Long-form Identifiermindat:1:5:6114:2
GUID0
Full ReferenceFanfani, 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
Plain TextFanfani, 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
In(1966) Mineralogical Magazine Vol. 36 (280) Mineralogical Society
Abstract/NotesSummarySome 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.

Mineral Pages

MineralCitation Details
Brackebuschite
Fornacite
Vauquelinite


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