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RB 61/00019 Report of gas from water bore, secn 8 Hd Kirkpatrick.
Gas was reported effervescing from a water bore of 256 feet depth near Ki Ki, South Australia. The water was sampled on May 11, 1965, but hydrocarbons were detected in the gas above the water in the sample bottle. There was a petroliferous smell from...-
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Published: 01 Jan 1961
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RB 77/00101 Hydrogeology of Rocky Gully Creek area, east of the Pallamanna Fault.
Three groundwater observation wells have been drilled at locations north-west of Murray Bridge to determine the effect of increased stream flows down the Rocky Gully and Preamimma Creeks. Rocky Gully Creek will be capable of accepting about 10 000 m...-
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Published: 01 Jan 1977
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RB 77/00132 Hydrogeology of the Paragum Depression, Monarto SA.
Cable tool and rotary drilling of 8 holes has enabled the geological sequence and general hydrology to be determined in the area to appraise its potential as a disposal site for stormwater runoff from urbanised Monarto.-
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Published: 01 Jan 1977
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RB 92/00015 Regional hydrogeology of the Loxton-Noora area, Murray Basin, South Australia.
The Loxton-Noora area is underlain by 3 aquifer systems - the Pliocene Sands water table aquifer, the confined Murray Group limestone and the deepest, the confined Renmark Group aquifer. Both confined aquifers contain groundwater of 20-25 000 mg/L...-
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Published: 01 May 1992
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RB 88/00055 Murray Basin hydrogeological investigation drilling programme, western margin (south). Progress report no. 7.
To investigate the effect of groundwater on River Murray salinity, 10 observation wells were completed in the Renmark Group confined aquifer and 1 in shallow basement near Swan Reach. Depths vary from 31 to 174 metres. Potentiometric surface varies...-
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Published: 01 Aug 1988
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RB 89/00049 Aspects of stratigraphy and structure in relation to the Woolpunda Groundwater Interception Scheme, Murray Basin, South Australia.
Micropalaeontological and biostratigraphic studies have been used. Groundwater flow systems were investigated near the Woolpunda Groundwater Interception Scheme (WGIS) - a major area of saline groundwater discharge to the Murray River. Structure was...-
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Published: 01 May 1989
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RB 75/00070 Recharge investigations, northern margin of the Milang Basin. Milang-Langhorne Creek area.
There is no abstract created for this record-
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Published: 01 Jan 1978
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RB 76/00107 Stratigraphy and engineering geology of the Monarto designated area - Monarto Development Commission.
Drilling of 25 cable tool holes to depth up to 20.1m in the designated area for Monarto New Town illustrates the nature, distribution and thickness of Quaternay and Tertiary sediments. The main tertiary units are the marine fossiliferous limestone of...-
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Published: 01 Jan 1976
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RB 2003/00013 North-western Murray Basin geological synthesis, South Australia.
The Murray Basin is an intracratonic basin filled with Cainozoic fluvial to shallow marine sediments. Deposition in the Eocene and early Oligocene was characterised by floodplain and swamp deposits, emplaced with occasional interbeds of shelly clays...-
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Published: 01 Aug 2003
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RB 2000/00004 Mallee region groundwater modelling - Report no. 1.
A five-layer finite difference groundwater flow model (MODFLOW) was developed for the Mallee Region to determine the impacts of irrigation on water levels and salinities. The model was calibrated for steady-state conditions over the entire modelled...-
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Published: 01 Feb 2000
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Marne River Catchment - Groundwater assessment.
The Marne River is a main tributary catchment for the River Murray, which generates ephemeral flows in wet years. Concerns have been expressed at the construction of large dams in the headwaters of the catchment, about their impacts on streamflow,...-
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