Middle-Upper Ordovician Shallow Platform to Deep Basin Transect, Southern Tasmania.
There is a profound change in sedimentary environment and in fauna going from the Middle-Upper Ordovician of Ida Bay to Surprise Bay over a present distance of only 25 km. The transition is from peritidal carbonates at Ida Bay, to subtidal carbonates at Precipitous Bluff to deep subtidal calcareous...
Main Authors: | , , , |
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Other Authors: | |
Format: | Book Part |
Language: | English |
Published: |
Oslo : Universitetsforlaget [University of Oslo]
1984
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Online Access: | https://eprints.utas.edu.au/11742/ https://eprints.utas.edu.au/11742/1/BurrettEtAl1984_SouthernTasmanianOrdovicianTransect.pdf |