Hostname: page-component-586b7cd67f-gb8f7 Total loading time: 0 Render date: 2024-11-26T06:38:52.474Z Has data issue: false hasContentIssue false

Amphibolite-granulite facies assemblages in southern Nyasaland

Published online by Cambridge University Press:  14 March 2018

S. W. Morel*
Affiliation:
67 The Rise, SevenoaksKent

Summary

The mineral assemblages developed in a variety of high-grade metamorphic rocks from southern Nyasaland are compared with standard metamorphic facies mineral assemblages proposed by some authors.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1961

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

Howie, ( R. A.) and Subramaniam, (A. P.), 1957. Min. Mag., vol. 31, p. 565.Google Scholar
Kennedy, (w. Q.), 1949. Geol. Mag., vol. 86, p. 43.CrossRefGoogle Scholar
Morel, (S. W.), 1955. Ibid., vol. 92, p. 241.Google Scholar
Morel, (S. W.) 1956. The geology of the Ncheu area. Rept. Geo. Surv. Nyasaland (unpubl.).Google Scholar
Morel, (S. W.) 1958. The geology of the Middle Shire area. Bull. Geol. Surv. Nyasaland, no. 10.Google Scholar
Ramberg, (H.), 1952. The origin of metamorphic and metasomatic rocks. Chicago (Chicago Univ. Press).Google Scholar
Turner, (F. J.) and Verhoogen, (J.), 1951. Igneous and metamorphic petrology. New York (McGraw-Hill).Google Scholar
Von Knorring, (O.) and Kennedy, (W. Q.), 1958. Min. Mag. vol. 31, p. 846.Google Scholar