The Benagerie Ridge is a basement high which has been actively shedding detritus since Adelaidean times. It includes porphyry, with thin cover of Adelaidean rocks, flanked by Cambrian and possible Adelaidean sediments. The Cainozoic blankets the...

Edeowie 1 (TD 984 metres), which aimed to identify a series of seismic reflectors mapped by SADME beneath the eastern Lake Torrens piedmont plain, has intersected a stratigraphic sequence with features indicating that complex structural changes occur...

Includes surface and subsurface stratigraphic data, and a geological map at 1:500 000 scale. 18 bores were re-logged.

The area mapped includes most of the area south of Lake Frome between the Flinders and Barrier Ranges, and part of the Olary Hills. Basin nomenclature has been revised for the Cainozoic. Drilling by CSR, Minad and Petromin NL has been used in the...

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Two major palaeodrainage systems of Tertiary age, with watersheds of up to 35 000 square km and channel lengths of 200-250 km, have been recognised and delineated using LANDSAT imagery, during 1:250 000 scale geological mapping in western South...

The widespread extent of silcretes in SA is demonstrated through stratigraphic relationships with palynologically dated sequences, and erosion of silcretes. The late Tertiary silcrete dominates the duricrusted landscape. Silica type varies according...

Age demonstrated by stratigraphic relationships with palynologically dated sequences, and evidence of erosion of silcretes.

Skeleton 2 penetrated sediments of the eastern Lake Eyre Basin, the Frome Embayment, and granitic basement of the Mount Painter Ridge. The hole records the southernmost known occurrence of Cadna-owie Formation in the Frome Embayment. Unexpectedly,...

Plant macrofossils from silicified Cainozoic fluvial sediments on CURDIMURKA occur in 2 discrete suites. One suite has been found only in outcrops of silicified Eyre Formation in the Poole Creek Palaeochannel. This suite and the macroflora of the...

A sample of carbonaceous mud was assigned a Middle Eocene age. The date also provides maximum age for the silcrete which indurates the upper part of the formation in the creek.

A PACE Initiative Year 3 subsidised drilling programme has been undertaken by the EL 3482 licensees over part of the Yarramba Palaeochannel north of the Honeymoon U deposit, seeking similar, Tertiary sediment-hosted roll-front uranium deposits in an...

The main aim of Havilah Exploration's PACE Initiative Year 3 approved drilling programme was to test the east-west trending, quartz-veined breccia zone that passes through the central Kalkaroo Dome, specifically in the footwall of the Kalkaroo Cu-Au...

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Southern Cross Resources Australia Pty Ltd (Southern Cross) purchased Rio Tinto Exploration Limited’s share of the Northern Olary Joint Venture, including its interest in the subject EL 2310 Yarramba, in November 2000. Southern Cross has held the...

An area centred ~50 km north-west of Olary is continuing to be explored for possible buried economic Prominent Hill or Olympic Dam type iron oxide associated copper-gold (IOCG) breccia style mineralisation. The area is considered highly prospective...

A very large area of the remote far north-east of the State was taken up early in 2008 by the unlisted Thorne-Clarke family company, to explore for sediment-hosted secondary uranium mineralisation of the type found in intracratonic sedimentary basins...

CURNAMONA PROVINCE SUMMARY Age: Sedimentation - late Palaeoproterozoic to early Mesoproterozoic. Felsic and mafic volcanism - late Palaeoproterozoic to early Mesoproterozoic. Granitic intrusion - late Palaeoproterozoic to early...

Diamond exploration in a region north to north-west of Oodnadatta comprised heavy mineral and geochemical sampling over magnetic anomalies selected from aeromagnetic surveys and further defined by ground magnetometry. Certain of this ground was...

Interpretation of historical drilling and mapping data from four separate small areas located from 40 to 90 km south-west of Lake Frome has indicated that these areas are shallowly underlain by Late Proterozoic basement. Such locations are deemed as...