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A Note on the Occurrence of Intergrowth between Diopsidic Augite and Albite and of Hydrogrossular from King Island, Tasmania

Published online by Cambridge University Press:  01 May 2009

Beryl Scott
Beryl Scott
Affiliation:
Geology Dept., University of Tasmania
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Abstract

A description is given of an intergrowth between augite and albite found in Spilitic lavas from King Island, Tasmania. Hydrogrossular is found pseudomorphing olivine and also in veins and vesicles in certain rocks of the same volcanic suite.

Type
Articles
Information
Geological Magazine , Volume 88 , Issue 6 , December 1951 , pp. 429 - 431
Copyright
Copyright © Cambridge University Press 1951

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References

REFERENCES

Benson, W. N., 1915. The Geology and Petrology of the Great Serpentine Belt of New South Wales: Part IV, The Dolerites, Spilites, and Keratophyres of the Nundle District. Proc. Linn. Soc. N.S. W., xl, 121–173.Google Scholar
Hutton, C. O., 1943. Hydrogrossular, A New Mineral of the Garnet-Hydrogarnet Series. Trans. Roy. Soc. N.Z., lxxiii, 174–180.Google Scholar
McConnell, D., 1942. Griphite, A Hydrophosphate Garnetoid. Amer. Min., xxvii, 452–461.Google Scholar
Scott, Beryl, 1951. The Petrology of the Volcanic Rocks of South-East King Island, Tasmania. Proc. Roy. Soc. Tasmania, 1950, 113–136.Google Scholar