Hostname: page-component-586b7cd67f-rcrh6 Total loading time: 0 Render date: 2024-11-24T23:15:25.447Z Has data issue: false hasContentIssue false
  • English
  • Français

Kyanite-Gneiss within a Thermal Aureole

Published online by Cambridge University Press:  01 May 2009

W. S. MacKenzie
Get access Rights & Permissions [Opens in a new window]

Abstract

This preliminary note records two discoveries in the Ross of Mull. Kyanite is considerably more widespread in the Moine rocks than previous investigations have indicated. Where the kyanite-gneiss enters the thermal aureole of the granite, large andalusite paramorphs are formed from kyanite.

Type
Articles
Information
Geological Magazine , Volume 86 , Issue 4 , August 1949 , pp. 251 - 254
Copyright
Copyright © Cambridge University Press 1949

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

Bosworth, T. O., 1910. Metamorphism around the Ross of Mull Granite. Quart. Journ. Geol, Soc., lxvi, 376.CrossRefGoogle Scholar
Clough, C. T., 1911. The Geology of Colonsay and Oronsay, with part of the Ross of Mull. Mem. Geol. Survey (Scotland).Google Scholar
Erdmannsdörffer, O. H., 1928. Über Disthen-Andalusitparagenesen. Sitz. Heidelberg. Akad. Wiss. Math.-naturwiss. Kl, Abh. 16.Google Scholar
Macgregor, A. G., 1928. Metamorphism around the Lochnagar Granite, Aberdeenshire. Rept. Brit. Assoc. (Glasgow, 1928), 553.Google Scholar
Tilley, C. E., 1935. The rôle of kyanite in the “ hornfels zone ” of the Carn Chuinneag granite (Ross-shire). Min. Mag., xxiv, 92.Google Scholar
von Eckermann, H., 1936. The Loos-Hamra region. Geol. Fören. Förh. (Stockholm), 58, 129.CrossRefGoogle Scholar