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Please use this identifier to cite or link to this item: https://nswdpe.intersearch.com.au/nswdpejspui/handle/1/1311
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dc.contributor.authorBembrick C.S-
dc.contributor.authorGilligan L, B-
dc.date.accessioned2023-06-21T10:01:29Z-
dc.date.available2023-06-21T10:01:29Z-
dc.date.issued1972en
dc.identifier.issn0155-3410-
dc.identifier.urihttps://nswdpe.intersearch.com.au/nswdpejspui/handle/1/1311-
dc.description.abstractThe 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.-
dc.relation.ispartofseriesQuarterly Notes-
dc.source/mnt/conversions/nswdpe/20220815_1_DPIE//Scanned Files/Box 32/Quarterly Notes 9 Geological Survey of New South Wales 1st October 1972.pdfen
dc.subjectCoila Basalten
dc.subjectIronstone Mogo and Bodallaen
dc.titleThe Coila Basinen
dc.titleGeochemical sampling of the ironstone at Corona. Broken Hill District-
dc.title.alternativeQuarterly Notes 9 Geological Survey of New South Wales 1st October 1972-
dc.title.alternativeQuarterly Notes 9-
dc.typepdfen
dc.contributor.corpauthorDepartment of Mines-
dc.contributor.corpauthorGeological Survey of NSW-
Appears in Collections:Geological Survey of NSW [1874 -present]

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