A Note on the Occurrence of Intergrowth between Diopsidic Augite and Albite and of Hydrogrossular from King Island, Tasmania
- 1 December 1951
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 88 (6) , 429-431
- https://doi.org/10.1017/s0016756800069983
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.Keywords
This publication has 1 reference indexed in Scilit:
- The geology and petrology of the Great Serpentine Belt of New South Wales. Part iv. The dolerites, spilites, and keratophyres of the Nundle districtProceedings of the Linnean Society of New South Wales, 1915