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Geology of central western Tasmania

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Corbett, KD, Green, GR and Williams, PR 1977 , 'Geology of central western Tasmania' , Papers and Proceedings of the Royal Society of Tasmania, vol. Landsc , pp. 7-28 , doi: 10.26749/rstpp.111.1.7.

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Abstract

The Queenstown-Zeehan-Rosebery area is geologically complex. It lies on a belt of folded Ecocambrian and early Palaeozoic rocks which were deposited in the Dundas Trough, a rift structure which developed between the metamorphosed Precambrian rocks of the Cradle Mountain- Frenchmans Cap area ( Tyennan Nucleus ) to the east and the relatively unmetamorphosed Proterozoic rocks of t he Rocky Cape Geanticline to the west .

Item Type: Article
Authors/Creators:Corbett, KD and Green, GR and Williams, PR
Keywords: Royal Society of Tasmania, RST, Van Diemens Land, natural history, science, ecology, taxonomy, botany, zoology, geology, geography, papers & proceedings, Australia, UTAS Library
Journal or Publication Title: Papers and Proceedings of the Royal Society of Tasmania
ISSN: 0080-4703
DOI / ID Number: 10.26749/rstpp.111.1.7
Collections: Royal Society Collection > Papers & Proceedings of the Royal Society of Tasmania
Additional Information:

Edited by M.R. Banks and J.B. Kirkpatrick. - Copyright Royal Society of Tasmania

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