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...

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Bibliographic Details
Main Authors: Burrett, CF, Stait, B, Sharples, C, Laurie, JR
Other Authors: Brunton, DL
Format: Book Part
Language:English
Published: Oslo : Universitetsforlaget [University of Oslo] 1984
Subjects:
Ida
Online Access:https://eprints.utas.edu.au/11742/
https://eprints.utas.edu.au/11742/1/BurrettEtAl1984_SouthernTasmanianOrdovicianTransect.pdf