Library Open Repository
Formations close to the Permo-Triassic boundary in Tasmania
Banks, MR and Naqvi, IH (1967) Formations close to the Permo-Triassic boundary in Tasmania. Papers and Proceedings of the Royal Society of Tasmania, 101. pp. 17-31. ISSN 0080-4703
1967_Banks_Formations_Permo-Triassic_boundary.pdf | Download (620kB)
Available under University of Tasmania Standard License.
The Cygnet Coal Measures is a unit of carbonaceous shale, coal and feldspathic sandstone in Tasmania of Upper Permian age. It is overlain gradationally or disconformably by the Springs Sandstone, the lower member of which, Barnetts Sandstone, is a thinly-bedded, fine-grained feldspathic to arkosic sandstone, and the upper, the Mountain Lodge Sandstone and a more thickly-bedded, medium-grained protoquartzite. The upper part of the Springs Sandstone is probably Otoceratan. The Permo-Triassic boundary lies within these gradational non-marine units and cannot yet be fixed accurately. The base of the Mountain Lodge Member is probably the most convenient boundary to use as the Permo-Triassic boundary in local field mapping.
|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|
|Page Range:||pp. 17-31|
|Additional Information:||Copyright Royal Society of Tasmania|
|Date Deposited:||29 May 2012 01:50|
|Last Modified:||18 Nov 2014 04:37|
|Item Statistics:||View statistics for this item|
Repository Staff Only (login required)
|Item Control Page|