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https://nswdpe.intersearch.com.au/nswdpejspui/handle/1/1311| Title: | The Coila Basin Geochemical sampling of the ironstone at Corona. Broken Hill District |
| Other Titles: | Quarterly Notes 9 Geological Survey of New South Wales 1st October 1972 Quarterly Notes 9 |
| Authors: | Bembrick C.S Gilligan L, B Department of Mines Geological Survey of NSW |
| Keywords: | Coila Basalt;Ironstone Mogo and Bodalla |
| Issue Date: | 1972 |
| Series/Report no.: | Quarterly Notes |
| Abstract: | The Coila Basalt is an olivine basalt flow of Middle Oligocene age overlying the Bergalia Formation and underlying the Meringo Creek Formation. It occurs as disconnected outcrops between Mogo and Bodalla, and fifteen stratigraphic sections show that it has a maximum thickness of 33 m and dips gently seaward. |
| URI: | https://nswdpe.intersearch.com.au/nswdpejspui/handle/1/1311 |
| ISSN: | 0155-3410 |
| Appears in Collections: | Geological Survey of NSW [1874 -present] |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| Quarterly Notes 9 Geological Survey of New South Wales 1st October 1972.pdf | Quarterly Notes 9 Geological Survey of New South Wales 1st October 1972.pdf | 3.9 MB | Adobe PDF |  View/Open |
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