Abstract
THE wide occurrence of the three aluminium silicate minerals andalusite, kyanite and sillimanite either individually or in pairs, or sometimes all together in metamorphic rocks1,2, makes the study of these minerals attractive to petrologists and experimentalists because their presence and associations may be used to delineate the temperature and pressure range of a given metamorphism.
Similar content being viewed by others
Article PDF
References
Hietanen, A., Amer. Mineral., 41, 1 (1956).
Pitcher, W. S., in Controls of Metamorphism (Edinburgh, 1965).
Pitcher, W. S., and Read, H. H., Quart. J. Geol. Soc. Lond., 116, 1 (1960).
Pitcher, W. S., and Spencer, M. O., Proc. Geol. Soc. Lond., No. 1654, 332 (1963).
Nagger, M. H., and Atherton, M. P., J. Petrol. (in the press).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
NAGGER, M., ATHERTON, M. & PITCHER, W. Composition of some Aluminium Silicate Bearing Contact Rocks from County Donegal, Eire. Nature 226, 841 (1970). https://doi.org/10.1038/226841a0
Received:
Issue Date:
DOI: https://doi.org/10.1038/226841a0
Comments
By submitting a comment you agree to abide by our Terms and Community Guidelines. If you find something abusive or that does not comply with our terms or guidelines please flag it as inappropriate.