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Gradational benthic marine communities in the Early Carboniferous...
Four benthic marine fossil commumtles are recognised in faunas of the Rhipidomella fortimuscula brachiopod Zone of late Visean (Early Carboniferous) age using multivariate... -
The Great Artesian Basin, Australia
The Great Artesian Basin occupies 1.7 X 10^6 km^2, or about one-fifth of Australia, extending across parts of Queensland, New South Wales, South Australia, and the Northern... -
Palynostratigraphy of the central west Murray Basin
Palynological analyses have been undertaken on four fully cored boreholes in the central west Murray Basin (Woodlands-1, Manilla-I, Piangil West-2 and Hatfield-1 holes) to... -
The "Geera Clay equivalent": a regressive marine unit in the Renmark Group...
Sandy clays deposited during the waning phase of Oligocene-Middle Miocene transgression of the Murray Basin conformablyoverlie the shallow to marginal marine Geera Clay and... -
The use of sediments to assess environmental impact on a large coastal...
Sediment samples (140) acquired from the estuarine and fluvial sections of the Hawkesbury River between Windsor (130 km from the coast) and Broken Bay have been analysed for... -
Structure and hydrocarbon potential of the Bremer Basin, southwest Australia
The Bremer Basin underlies part of the upper continental slope of offshore southwest Australia. It occupies an area of 9000 km2, and contains a sedimentary pile probably 10 km... -
Source rock potential and hydrocarbon prospectivity of the Darling Basin, NSW
Available geological and geophysical data for the dominantly Devonian Darling Basin of western New South Wales indicate a high risk for petroleum exploration. Hydrocarbon... -
Great Artesian Basin - Geomorphology
This dataset classifies the geomorphological features of the GAB and includes the offshore extents of the GAB beneath the Gulf of Carpentaria. The geomorphological... -
Marine benthic communities in the Early Carboniferous of New South Wales...
The Delepinea aspinosa brachiopod Zone comprises two subzones: the Inflatia elegans and Linoprotonia tenuirugosa Subzones. Multivariate (cluster) analysis is used to identify... -
Upper Cambrian (Mindyallan) trilobites and stratigraphy of the Kayrunnera...
Nine species of trilobites are recorded from three localities within a restricted stratigraphic interval near the base of the newly defined Kayrunnera Group (previously... -
Sedimentary cycles in the Surat Basin and global changes of sea level
Six sedimentary cycles, each hundreds of metres thick, have been recognised in the Surat Basin. The Jurassic cycles (nos. 1-4) typically started with high-energy deposition of... -
Stratigraphy and sedimentology of Late Palaeozoic glaciomarine sediments...
Sediments of the Late Palaeozoic Urana Formation in infrabasins beneath the Cainozoic Murray Basin include glaciomarine diamictite, fine-grained sediment, sandstone, and... -
Palynostratigraphy of the Bookpurnong Beds and related Late Miocene-Early...
Dinoflagellates offer a reliable method for distinguishing the Late Miocene-Early Pliocene Bookpurnong beds from lithologically similar marginal marine sediments, such as the... -
The Great Cumbung Swamp - terminus of the low-gradient Lachlan River,...
The Lachlan River rises in the humid highlands of southeastern Australia and flows westward into the Murray Basin. The climate is sub-humid to semi-arid and, as it crosses the... -
Thick ferromanganese deposits from the Dampier Ridge and the Lord Howe Rise...
Chemical and mineralogical data are presented for four ferromanganese samples (two nodules and two crusts) from two stations of the West German vessel Sonne. Three samples came... -
The Ivanhoe Block-its structure, hydrogeology and effect on groundwaters of...
The Ivanhoe Block is a faulted and uplifted concealed basement ridge complex underlying the mallee sand dunes adjacent to the New South Wales part of the Western Riverine Plain... -
Lord Howe Rise, Tasman Sea - preliminary geophysical results and petroleum prospects
The Lord Howe Rise is a major submarine feature in the Tasman Sea; it extends northwest from the New Zealand continental margin and lies about 600 to 1200 km off the east coast... -
Evidence of an exhalative origin for deposits of the Cobar district, New South Wales
Evidence is presented to show that a strong mineralogical/chemical zoning exists in seven deposits of the Cobar-Nymagee area. Characteristically, the within-deposit zoning,... -
Vegetation and climate of the late Cainozoic in the Murray Basin and their...
The Murray Basin was forested throughout the Tertiary, becoming open woodlands and grasslands in Plio-Pleistocene time. Precipitation was very high through the early Tertiary,... -
Diagenesis of Jurassic and Lower Cretaceous sandstones of the Eromanga Basin...
The Jurassic and Lower Cretaceous sandstones of the Eromanga Basin in New South Wales can be divided into quartzose and volcanolithic petrofacies. The latter comprises...