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Formations close to the Permo-Triassic boundary in Tasmania

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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

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Abstract

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.

Item Type: Article
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
ISSN: 0080-4703
Additional Information: Copyright Royal Society of Tasmania
Date Deposited: 29 May 2012 01:50
Last Modified: 18 Nov 2014 04:37
URI: http://eprints.utas.edu.au/id/eprint/14251
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