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ExpNotes CURDIMURKA: Explanatory Notes CURDIMURKA
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ExpNotes POOLOWANNA: Explanatory Notes POOLOWANNA
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Bull 040 Cretaceous Biostratigraphy of the Great Artesian Basin in South Australia
After its formation as a single sedimentary entity the Great Artesian Basin provided a marine environment only during the Cretaceous Aptian, Albian and early Cenomanian in South Australia. Santos' Oodnadatta 1 well (1957), continuously cored through...-
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RB 70/00100 Reconnaissance survey and photo-geological interpretation Gason Dome area of the Great Australian Artesian Basin, South Australia.
The GASON 1:250,000 map area is located in the northeast of South Australia, on the Birdsville Track. The map area includes the Gason, Dome, a topographically low structure with a northeasterly trending axis, and shallow dips on its flanks. The Upper...-
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Published: 24 Jul 1970
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RB 71/00142 Upper Cretaceous palynology of the Winton Formation, GASON 1:250 000 sheet.
Cores yielded well preserved and diverse microflora of the Tricolpites pannosus zone of Albian (?) Cenomanian age. Core from Gason 2 reflects restricted, possibly swamp, environment, whereas the other cores represent lacustrine sedimentation. Recycled...-
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Published: 06 Sep 1971
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RB 70/00154 Palaeontological examination of outcrop samples KOPPERAMANNA 1:250 000, sheet 1. Cretaceous rocks.
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Published: 01 Jan 1970
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RB 73/00096 Explanatory Notes for the GASON 1:250 000 geological map.
The Gason 1:250 000 sheet area is centred about 850 km north of Adelaide, in the South Australian portion of the Great Artesian Basin. The area mapped includes most of the Gason Dome, a gentle upwarp in a relatively flat-lying sequence of Mesozoic and...-
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Published: 12 Apr 1973
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RB 73/00026 Measured sections from the INNAMINCKA 1:250 000 area.
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Published: 31 Jan 1973
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RB 73/00161 Explanatory Notes for the NOOLYEANA 1:250 000 geological map.
The NOOLYEANA 1:250 000 sheet area lies in the northern portion of the Great Artesian Basin in South Australia. The area mapped includes the southern part of the Simpson Desert and the very northern end of Lake Eyre North. The oldest outcrops in the...-
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Published: 03 Jul 1973
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RB 73/00043 Explanatory Notes for the PANDIE PANDIE 1:250 000 geological map.
The PANDIE PANDIE 1:250 000 map area lies in the most northerly portion of the Great Artesian Basin in South Australia. The western half of the area is covered by the longitudinal dunes of the Simpson Desert, while the remainder is covered by (a) the...-
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Published: 14 Feb 1973
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RB 63/00064 Stratigraphy of the Chowilla area, South Australia.
This report deals with the stratigraphy and sedimentary history of the Chowilla area in the Murray Basin. Local geology is set against a background of geological information derived from other areas in southern Australia. Local stratigraphy is based...-
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Published: 01 Jan 1966
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RB 74/00204 Sampling and measurement of Great Artesian Basin mound springs, South Australia. Progress report 1, Dalhousie Springs.
Discharge from visited springs in the Dalhousie area was estimated at .86 cumecs. There may be as much as .02 cumecs additional seepage through many smaller seeps in the area which were not visited. The spring waters were alkaline, with a pH varying...-
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Published: 01 Jan 1974
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RB 73/00245 Explanatory Notes for the LAKE EYRE 1:250 000 geological map.
The LAKE EYRE 1:250 000 sheet area is located about 750 km north of Adelaide on the south-western margin of the Great Artesian Basin. The map area incorporates 15 950 square km, with Lake Eyre itself covering about half of this area. The oldest...-
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Published: 18 Oct 1973
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RB 73/00248 Explanatory Notes for the KOPPERAMANNA 1:250 000 geological map. Stratigraphic sections and comments on the Cenozoic rocks
The KOPPERAMANNA map area covers arid stony tableland and sandridge desert on the Birdsville Track, in the Great Australian Artesian Basin about 100 km north of Marree and to the east of Lake Eyre, South Australia. The Cooper Creek crosses the area...-
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Published: 22 Oct 1973
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RB 74/00025 Geology of the FROME 1:250 000 geological map and adjacent regions.
The Frome 1: 250 000 map covers the northern part of the South Australian portion of the Frome Embayment. The embayment is essentially the eastern portion of a Mesozoic basin, developed on Palaeozoic and Precambrian rocks during Upper Jurassic time by...-
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Published: 01 Jan 1974
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RB 74/00028 Explanatory Notes for the POOLOWANNA 1:250 000 geological map.
The POOLOWANNA 1:250 000 sheet area is located about 1000 km north of Adelaide, in the extreme north of the South Australian part of the Great Artesian Basin. It is entirely covered by the central southern end of the Simpson Desert. The oldest mapped...-
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Published: 30 Jan 1974
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Round Hill and Nillinghoo. Annual reports, joint annual reports and final report to licences' joint surrender, for the period 30/9/2009 to 19/2/2014.
Afmeco Mining and Exploration Pty Ltd is exploring for possible economic sedimentary uranium mineralisation which may have formed within permeable sand units of the Tertiary Callabonna Sub-basin. The subject ELs 4317 and 4318 are part of 7-licence...-
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Published: 24 Nov 1911
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Trooper Nob area. Annual report and final report to licence expiry/full surrender, for the period 11/7/2011 to 10/7/2013.
A substantial area (~50 square km in extent) of unusual surface ironstone enrichment on the Quaternary peneplain lying to the east of Etadunna Homestead on the southern Birdsville Track was investigated for its possible economic potential as a source...-
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Published: 08 Feb 1914
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Cooinchina Creek (synonym: the West Lake Eyre Project). Annual reports and final report to licence expiry/full surrender, for the period 21/9/2007 to 20/9/2010.
An area located approximately 50 km east of William Creek and abutting the western shoreline of Lake Eyre North was taken up to explore for possible concealed IOCG style base metal and uranium deposits, that could have formed in buried Archaean to...-
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Published: 30 Jun 1910
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Warana Hill - Areas 1-3. Joint annual reports to licences' joint expiry/full surrender, for the period 30/6/2009 to 29/6/2011.
A conjoined multi-licence area located in the northern Strzelecki Desert, centred approximately 110 km north-northwest of Moomba, has been explored for possible economic buried Cenozoic heavy minerals sands (HMS) deposits, and also for shallow...-
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