The Metamorphism of the Pre-Cambrian Dolomites of Southern Eyre Peninsula, South Australia
- 1 November 1920
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 57 (11) , 492-500
- https://doi.org/10.1017/s0016756800106922
Abstract
THE rocks arising from the metamorphism of the more impure dolomitic sediments are calc-magnesian silicate types in which all carbon dioxide has been expelled. In some of the rocks to be described it is clear that superposed on the normal metamorphism there has been a metamorphism by addition of material from the neighbouring magma.Keywords
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