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Spherically arranged inclusions in post-tectonic garnet porphyroblasts

Published online by Cambridge University Press:  05 July 2018

P. K. Harvey  and
C. C. Ferguson
P. K. Harvey
Affiliation:
Department of Geology, Nottingham University
C. C. Ferguson
Affiliation:
Department of Geology, Nottingham University
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Summary

Garnet porphyroblasts, containing elongate ilmenite inclusions arranged in an essentially spherical pattern, are described. The garnets are post-tectonic, and the inclusion pattern is the result of deformation and simultaneous replacement of the matrix by the growing porphyroblast.

Type
Research Article
Information
Mineralogical Magazine , Volume 39 , Issue 301 , March 1973 , pp. 85 - 88
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1973

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References

Cruse, (M. J. B.) and Leake, (B. E.)s 1968. Proc. Roy. Irish Acad., 67, Sect. B, No. 1, 1–36.Google Scholar
Ferguson, (C.C.) and Harvey, (P.K.), 1972. GeoL Soc. Amer. Bull., 83, 3 39–40.CrossRefGoogle Scholar
Misch, (P.), 1969. Amer. Journ. Sci., 267, 43–63.CrossRefGoogle Scholar
Misch, (P.) 1971. GeoL Soc. Amer. Bull., 82, 245–52.Google Scholar
Misch, (P.) 1972. Ibid. 83, s-2.CrossRefGoogle Scholar
Powell, (D.) and Treagus, (J. E.), 1970. Min. Mag., 37, 801–14.CrossRefGoogle Scholar