Hostname: page-component-cd9895bd7-jkksz Total loading time: 0 Render date: 2024-12-23T19:54:05.344Z Has data issue: false hasContentIssue false
  • English
  • Français

A note on the relationship of sillimanite to biotite

Published online by Cambridge University Press:  01 May 2009

David Shelley
David Shelley
Affiliation:
Department of Geology, University of Canterbury, Christchurch, N.Z.
Get access Rights & Permissions [Opens in a new window]

Summary

A description is given of potassium feldspar which was produced during the fibrolitization of biotite.

Type
Articles
Information
Geological Magazine , Volume 105 , Issue 6 , December 1968 , pp. 543 - 545
Copyright
Copyright © Cambridge University Press 1968

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

Chinner, G. A. 1961. The Origin of Sillimanite in Glen Clova, Angus. J. Petrology, 2, 312–323.CrossRefGoogle Scholar
Chinner, G. A. 1966. The significance of the aluminium silicates in metamorphism. Earth—Sci. Rev., 2, 111–126.CrossRefGoogle Scholar
Cogné, J. & Shelley, D. 1966. Structure géologique du secteur des Abers (Nord Finistére). Bull. Serv. Carte géol. Als. Lorr., 19, 1–40.Google Scholar
Francis, G. H. 1956. Facies Boundaries in Pelites at the Middle Grades of Regional Metamorphism. Geol. Mag., 93, 353–368.CrossRefGoogle Scholar
Tozer, C. F. 1955. The Mode of Occurrence of Sillimanite in the Glen District, Co. Donegal. Geol. Mag., 92, 310–320.CrossRefGoogle Scholar
Watson, J. 1948. Late Sillimanite in the Migmatites of Kildonan, Sutherland. Geol. Mag., 85, 149–162.CrossRefGoogle Scholar