The Structure of the bedded rocks west of Rosebery, Tasmania
- 1 January 1967
- journal article
- research article
- Published by Taylor & Francis in Journal of the Geological Society of Australia
- Vol. 14 (2) , 333-337
- https://doi.org/10.1080/00167616708728670
Abstract
The Rosebery “Series”, due west of Rosebery, Tasmania, dips west and is the right way up. Along strike to the north and south there are marked changes in rock type, and possibly infolding and interbedding of sediments similar to the Crimson Creek Argillite. The Rosebery “Series” is younger than part of the Mount Read Volcanics, which may imply that some of the Volcanics are equivalent to the Oonah Quartzite and Slate.Keywords
This publication has 2 references indexed in Scilit:
- Palaeozoic tectonism, sedimentation and mineralization in West TasmaniaJournal of the Geological Society of Australia, 1963
- The Precambrian rocksJournal of the Geological Society of Australia, 1962