Petrography of rocks from the Western Chain of the Snares Islands (Note)
- 1 May 1975
- journal article
- brief note
- Published by Taylor & Francis in New Zealand Journal of Geology and Geophysics
- Vol. 18 (3) , 491-499
- https://doi.org/10.1080/00288306.1975.10421549
Abstract
The Western Chain of the Snares Islands consists mainly of jointed muscovite granite, which locally is strongly crushed. Previously described fragments of schist from Rua islet are possibly remnants of roof pendants; they are further discussed. The schist includes varieties with biotite and muscovite and with biotite alone, and these rocks appear to be similar to schists of the Tin Range, Stewart Island. A secondary (hydrothermal) origin for much of the abundant muscovite of the Western Chain granite is suggested.Keywords
This publication has 4 references indexed in Scilit:
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- Alteration of biotite under mesothermal conditionsEconomic Geology, 1958
- The Finer-Grained Calcalkaline Granites of New EnglandThe Journal of Geology, 1952
- A Granite-Schist Contact in Stewart Island, New ZealandQuarterly Journal of the Geological Society, 1934