Ediacaran events: boundary relationships and correlation of key sections, especially in ‘Armorica’
Abstract The transitional interval between the Adelaidean and Ediacaran systems in the central Flinders Ranges, South Australia, comprises mainly basinal sediments, with some tuff beds (Bunyeroo Formation) and a widespread thin dolomite bed which apparently evidences a brief regressive episode (base...
| Published in: | Geological Magazine |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Cambridge University Press (CUP)
1984
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| Online Access: | http://dx.doi.org/10.1017/s0016756800030788 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800030788 |