Skip to main content
Log in

Synthesis and Properties of Piemontite

  • Letter
  • Published:

From Nature

View current issue Submit your manuscript

Abstract

THE simplest member of the epidote group, the calcium, aluminium end-member, has the structural formula Ca2Al.AlOH.AlO.Si2O7.SiO4 (ref. 1); common epidote forms through the replacement of part of the aluminium by ferric iron, and in the piemontites manganese is also present. The aluminium, iron and manganese end-members will be written Cz, Ps and Pm respectively. Common epidote is approximately Cz70Ps30, and piemontitos range from Cz76Ps22Pm2 to Cz40Ps13Pm47.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  1. Ito, J., Morimoto, N., and Sadanaga, R., Acta Cryst., 7, 53 (1954).

    Article  CAS  Google Scholar 

  2. Seki, Y., Amer. Min., 44, 720 (1959).

    CAS  Google Scholar 

  3. Malmqvist, D., Bull. Geol. Inst., Uppsala, 22, 223 (1929).

    Google Scholar 

  4. Zambonini, F., Mineral. Abstr., 2, 188 (1921).

    Google Scholar 

  5. Edwards, A. B., Baker, G., and Callow, K. J., J. Geol. Soc. Austral., 3, 55 (1956).

    CAS  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

STRENS, R. Synthesis and Properties of Piemontite. Nature 201, 175–176 (1964). https://doi.org/10.1038/201175a0

Download citation

  • Issue Date:

  • DOI: https://doi.org/10.1038/201175a0

  • Springer Nature Limited

This article is cited by

Navigation