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Vesuvianite and Grossular as Products of Regional Metamorphism

Published online by Cambridge University Press:  01 May 2009

C. E. Tilley
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Extract

The chemical environment of vesuvianite and grossular is typically revealed in their associated minerals, calcite, diopside, scapolite, and wollastonite, characteristically developed under the physical conditions prevailing in thermal metamorphism.

Type
Original Articles
Information
Geological Magazine , Volume 64 , Issue 8 , August 1927 , pp. 372 - 376
Copyright
Copyright © Cambridge University Press 1927

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References

page 374 note 1 Wollastonite as a constituent of a grossular-vesuvianite-diopside-microcline assemblage is once recorded from the limestone of the Carie Burn.

page 375 note 1 Geol. Mag., Vol. LVIII, 1921, p. 307.Google Scholar

page 375 note 2 Loc. cit.

page 376 note 1 Kolderup, N. H., “Die Injektionsmetamorphose des Dolomitmarmors im Mögstergebiet in westlichen Norwegen,” Bergens Museums Aarbok, 1923–1924, Naturvidensk. raekke, Nr. 1.Google Scholar