posted on 2023-11-02, 06:17authored byPR 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 .
History
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.