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Geology of central western Tasmania

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posted on 2023-11-02, 06:17 authored by PR Williams, GR Green, KD Corbett
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 .

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Publication title

Papers & Proceedings of the Royal Society of Tasmania

Volume

Landsc

Pagination

07-28

ISSN

0080-4703

Rights statement

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

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