Palynological analyses of nine grab samples from the Lochiel coal test pit show two distinct floristic types, i.e. Haloragacidites spp. dominated and Nothofagidites spp. dominated palynofloras. This distinction is interpreted as indicating a change...

The rural township of Kangarilla currently has no reticulated water supply system or common effluent disposal scheme, so instead its residents' potable water supplies are obtained from domestic rainwater tanks, and garden water is generally drawn...

Cambro-Ordovician Warburton Basin strata and intrusive granites are conventionally regarded as the economic basement beneath the Cooper-Eromanga oil and gas province in northeastern South Australia and southwestern Queensland. This study, the first...

A combined groundwater and solute transport model (MODFLOW and MT3D) was constructed of the Loxton Irrigation Area to determine the future impacts on groundwater levels and salt loads to the river and floodplain for a range of local irrigation...

Samples are identified from Late Cretaceous to Early Eocene.

Major resources of magnesite are included as sedimentary interbeds within Late Proterozoic Skillogalee Dolomite which extends the length of the Geosyncline for 820 km. Magnesite interbeds are best developed from Leigh Creek to the Willouran Ranges,...

Three grab samples of calcareous concretions were assigned an Early Aptian age.

Three drill cuttings samples were assigned a Late Eocene age.

A sample of carbonaceous mud was assigned a Late Eocene age.

Ten outcrop samples, including carbonaceous muds, siltstone and limestone concretions, were collected as part of a study of Early Cretaceous palaeoclimate. The samples were all of Bulldog Shale from a shallow water marine environment, except for...

Drill core from samphire and mangrove marshes north of Gillman - Wingfield are used to interpret the shallow sub-surface stratigraphy of the region. A Holocene marine sequence up to 8 metres thick overlies Late Pleistocene alluvial (Pooraka Formation)...

Four horizons were mapped (top of basement, top of Permian, top of Cretaceous and Sea Floor). The Denman Basin is a 50 km wide, north-south trending depression in Early Palaeozoic - Precambrian bedrock, infilled with up to 400 metres of Permian...

The Duntroon Basin is located in the centre of the Southern Rift System between the Bight and the Otway Basins, west and SW of Kangaroo Island. It is limited to the north by the Proterozoic Gawler Craton. The formation of the basin is related to the...

This study is part of a joint SADME / BMR study, and details exploration history and interpretation of the "outer" Duntroon Basin, tying in a previous regional interpretation of the Otway Basin to interpretations of co-workers in the Bight and "inner"...

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The offshore extension of the Eden-Burnside Fault has been mapped from shallow-penetration seismic reflection profiles. Between Hallett Cove and Port Noarlunga, it parallels the coastline 2 km offshore. The fault separates a coastal platform of thin,...

The Cainozoic Eucla Basin has been the focus of recent heavy mineral exploration due to the recognition of Tertiary coastal features including the Ooldea Range. Hypsometric and Landsat data, together with detailed work on the Tertiary stratigraphy of...

A transient electromagnetic survey was done over several salina locations at Tumby Bay to assist in evaluating dryland salinity problems. The survey findings were useful in mapping subsurface saline groundwater and basement topography, and clearly...

Sediments analysed from VB06 and VB07 are correlative with an early phase of the Garford Formation, either in the Middle Miocene or the Early Miocene. The environment of deposition appears to have been fairly open marine, or at least an estuarine...

A sample examined from the CAR03-1 exploration drillhole is Late Eocene in age and correlative with the marginal marine upper part of the Pidinga Formation.