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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,... -
A non-marine Lower Cretaceous rift-related epiclastic volcanic unit in...
The Early Cretaceous non-marine volcaniclastic Eumeralla Formation accumulated in a rift basin on the southern margin of Australia during the break-up of eastern Gondwana.... -
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... -
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... -
A non-marine Lower Cretaceous rift-related epicIastic volcanic unit in...
Relationships, thicknesses, and palaeocurrent and other sedimentary data applying to facies associations in Eumeralla Formation outcrops in the eastern Otway Basin distinguish... -
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... -
Global sea-level change as a method of correlating the Late Permian coal...
Eustatic changes in sea level can be used to correlate sequences in widely separated areas. Thick terrestrial sequences with marine intercalations are especially suitable,... -
The hydrogeochemistry of groundwater in fractured bedrock aquifers beneath...
Fresh to brackish groundwaters in the range of 250 to 2250 mglL occur in fractured bedrock aquifers beneath dryland salinity sites at Yass in the Southern Tablelands of New... -
Sequence analysis and depositional models of crinoidal limestones, Permian...
The Permian Yessabah Limestone, a thick crinoidal limestone unit, appears abruptly in the stratigraphic succession over a large area of the Hastings Block in northeastern New... -
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... -
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... -
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... -
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,... -
Stratigraphy and sedimentology of mid-Tertiary permeability barriers in the...
In the Murray Basin of southeastern Australia, the accelerated emergence of groundwater-related salinity problems in recent decades has led to the realisation that future... -
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... -
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... -
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 "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... -
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,... -
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...