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RB 92/00045 Upper South-East dryland salinity and flood management plan. Excavation characteristics and slope design for the drainage channels.
The Upper South-East Dryland Salinity and Flood Management Plan proposals aim to address the worsening salinisation problems now clearly visible in the area. This report provides feasibility and preliminary project design data to the EWS engineers who...-
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Published: 01 Sep 1992
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RB 97/00039 Lineament tectonic data, South Australia, with a focus on the Cooper Basin.
The lineament mapping methods used by E.S.T. (Tim) O'Driscoll, which were a crucial factor in the discovery of Olympic Dam, the world's largest known Cu-U-Au-Ag deposit, and of several other lesser Australian metallic orebodies, have now been applied...-
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Published: 01 Oct 1997
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EPP 24, Otway Basin. Farmin evaluation report.
EPP 24 lies in the north-western corner of the Otway Basin, offshore from Robe, South Australia. The permit geology is dominated by sediments of the Early Cretaceous Otway Group. A tectonic hinge-line called the Chama Terrace runs obliquely from...-
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Katnook 2. Test reports.
Numerous analyses of Katnook 2 drilling results, well logs, open and cased- hole drillstem tests and extended production testing are discussed by various specialist reservoir engineering reports. Current conclusions are that testing so far of the...-
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1988 Lake Hawdon Seismic Survey. Final report.
AIM: To mature an intra-Pretty Hill Sandstone lead, which had been observed from the 1986 Lake Eliza Seismic Survey to exist as an unfaulted four-way dip closure within the downthrown fault block on the northern flank of the Lake Eliza High, and also...-
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Published: 01 Jan 1989
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Hydrocarbon potential of S87-1 application area, Otway Basin.
There is no abstract created for this record-
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Preliminary structural study of the Penola area, PEL 27, South Australia.
This report deals with the preliminary exploration-oriented structural analysis of a portion of PEL 27, i.e. the Penola area, based on interpretation of seismic survey data. The objectives of the study were to: analyse the three dimensional data...-
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1992 Beachport Seismic Survey. Reports for the period February to June 1992.
AIM: To acquire further detailed reflection seismic coverage of the south-west of the licence area to resolve doubts about the currently mapped closures on the following structures: (i) The Woakwine Prospect, a tilted fault block near the intersection...-
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PEL 60, Otway Basin, South Australia. Technical Committee meeting [presentation notes], 29th November 1998.
The licensee's current understanding of the petroleum geology and geophysics for the PEL 60 area is discussed (in the form of presentation slide montages) under the topic headings Churinga 1 post-audit, Prospectivity review, New mapping and Future...-
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Published: 29 Nov 1998
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Otway Basin, South Australia. Interpretation of Robe Trough aeromagnetic data.
Preview Resources Pty Ltd has interpreted and computer modelled selected anomalies in the aeromagnetic data in the Robe Trough area as a guide to structural interpretation of the total magnetic intensity data and pseudo-depth-slice data. This is a...-
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Published: 26 Oct 1995
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1997 Stockdale Seismic Survey. Reports for the period February 1997 to May 1998.
AIM: To further delineate the Stockdale lead, the Churinga Prospect, the Sugarloaf Prospect and several small fault bounded leads along the southern side of the central uplift zone of the onshore Robe Trough, with the expectation of then being able to...-
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RB 2000/00016 Groundwater flow model of the Tertiary confined sand aquifer in southeast South Australia and southwest Victoria.
A three-layered transient groundwater flow model of the Tertiary Confined Sand Aquifer (TCSA) underlying the South-East of South Australia and south-west region of Victoria has been constructed using MODFLOW software. The model is being used as a...-
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Published: 01 May 2000
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Vertical groundwater recharge to the Tertiary confined sand aquifer, South-East, South Australia.
Groundwater flows mainly through two major aquifer systems: a regionally unconfined aquifer, and an underlying confined aquifer. The two aquifers are separated by a low permeability confining bed (or aquitard). Determining the degree of hydraulic...-
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