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Abstract

The Sandfiy-Oyster Cove areas consist of Permian
and Triassic sediments which have been
widely intruded by dolerite in the form of sills and
dykes. The sills are so extensive that it appears unlikely
that any of the sedimentary exposures have
been left in their original stratigraphical positions.
Syenite dykes occur in the south of the area, and
two basalt outcrops have been mapped.

Item Type:	Article
Authors/Creators:	Rodger, TH
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
ISSN:	0080-4703
Collections:	Royal Society Collection > Papers & Proceedings of the Royal Society of Tasmania
Additional Information:	Copyright Royal Society of Tasmania
Item Statistics:	View statistics for this item

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