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Structural similarities of some secondary lead minerals

Published online by Cambridge University Press:  14 March 2018

L. Fanfani  and
P. F. Zanazzi
L. Fanfani
Affiliation:
Istituto di Mineralogia dell'Università di Perugia, Perugia (Italy)
P. F. Zanazzi
Affiliation:
Istituto di Mineralogia dell'Università di Perugia, Perugia (Italy)
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Summary

Some 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.

Type
Research Article
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 36 , Issue 280 , December 1967 , pp. 522 - 529
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1967

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References

Bideaux, (R. A.), Nichols, (M. C.), and Williams, (S. A.), 1966. Amer. Min., vol. 51, p. 258.Google Scholar
Cocco, (Cx.), Fanfani, (L.), and Zanazzi, (P. F.), 1966. Zeits. Krist., vol. 123, p. 321.CrossRefGoogle Scholar
Donaldson, (D. M.) and Bares, (W. H.), 1955. Amer. Min., vol. 40, p. 597.Google Scholar
Fanfani, (L.) and Zanazzi, (P. F.), 1967. Zeits. Krist., in press.Google Scholar
Nichols, (M. C.), 1966. Amer. Min., vol. 51, p. 267.Google Scholar