Middle-Upper Ordovician Shallow Platform to Deep Basin Transect, Southern Tasmania
Version 2 2025-02-12, 05:18
Version 1 2023-05-27, 23:55
chapter
posted on 2025-02-12, 05:18 authored by CF Burrett, B Stait, Christopher SharplesChristopher Sharples, J LaurieThere 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 shales at Pt. Cecil to deep water micrites, graptolitic shales and carbonate turbidites at Surprise Bay.-from Authors
History
Publication title
Aspects of the Ordovician SystemSeries
Palaeontological contributions from the University of OsloVolume
295Number
295Pagination
xx-xxISBN
8200063194Department/School
Geography, Planning and Spatial Sciences, Earth Sciences, Geography, Planning, and Spatial SciencesPublisher
University of Oslo, Series Palaeontological contributions from the University of Oslo no. 295Publication status
- Published
