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RB 90/00004 Foraminiferal dating of WH-1, Woorlo Hill transect, EL 1555.
Foraminiferal dating of marginal marine sediments intersected in WH1 drillhole was carried out to identify the age of the Tertiary drilling objective reached, a heavy mineral-bearing single stratum.-
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Published: 01 Jan 1990
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Koomooloo [Homestead] and Faraway Hill. Joint first progress report and joint final report to licences' full surrender, for the period 31/8/1990 to 28/3/1991.
TARGET: Possible economic heavy mineral sand deposits formed within the Pliocene Parilla Sand sequence along the north-western margin of the Murray Basin, both in the Canegrass area and the area east of Braemar Station. EXPLORATION: A consultant's...-
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RB 2022/00003 Zircon provenance and sedimentary transport processes – implications for the late Neogene evolution and heavy mineral deposits of the western Murray Basin, South Australia.
Strandlines or elevated shorelines, located across the Murray Basin in south-eastern Australia, trace the preserved remnants of former emergent coastlines that developed during the Late Miocene (c. 7 to 4 Ma) marine regression. Strandline traces...-
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Published: 01 May 2022
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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 2003/00009 Northern Murray Basin drilling and interpretations, 2001.
Stratigraphic drilling has been undertaken by PIRSA in the South Australian portion of the northern Murray Basin to investigate the stratigraphy and sedimentology of the Cainozoic sedimentary sequences, as well as the heavy mineral sand potential of...-
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Published: 01 Aug 2003
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RB 2015/00031 Provenance of zircon in heavy mineral sand deposits, western Murray Basin.
The Murray Basin in south-eastern Australia contains significant economic resources of heavy minerals (ilmenite, zircon, rutile) in coastal strandlines of a prograding sandplain that formed during marine regression in Late Miocene – Early Pliocene...-
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Published: 01 May 2016
