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RB 90/00077 Skeleton 2. Well completion report.
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,...-
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Published: 01 Dec 1990
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Data release - as updated [made at SA Director of Mines’ discretion] : Paralana Creek (part of the Beverley Project). Annual reports for the period 29/9/2009 to 15/11/2015.
Work undertaken on EL 4378 during the 2009-2010 reporting year included the drilling of 478 vertical rotary mud holes totalling 132,960 m, and core drilling totalling 4117 m performed in 16 of these holes for stratigraphic unit / resource...-
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Published: 24 Dec 1915
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SP 024 New Late Cainozoic Rock Units and Depositional Environments, Lake Frome Area,South Australia
There is no abstract created for this record-
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RB 75/00103 Stratigraphy sedimentology and uranium deposits of Tertiary rocks, Lake Frome area, SA.
There is no abstract created for this record-
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Published: 01 Jan 1975
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Lake Frome East. Progress and final reports to licence expiry for the period 13/11/79 to 12/5/80.
As part of a wider search over SA for possible continental salt lake occurrences of NaCO3-rich brines and of fossil crystalline trona beds, presumed to be equivalent to the Lake Magadi (Kenya) / Green River Basin (Utah - Wyoming) style Tertiary...-
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Published: 30 Apr 1980
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Woolatchi Creek. Progress, partial surrender and technical reports to licence surrender, for the period 12/4/1982 to 27/8/1985.
Diamond drillhole WC1 was drilled by Marathon to a total depth of 173.5 m over the Woolatchi Creek aeromagnetic anomaly, as part of an ongoing search for uranium and base metals in the north-eastern Flinders Ranges and Lake Frome Plains region....-
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Woolatchi Creek. Progress and annual reports for the period 20/2/80 to 11/4/83.
41 open-hole rotary drillholes (total 5999 metres) were drilled and geophysically logged to search for possible sedimentary uranium occurrences in the Early Cretaceous Parabarana Formation and in overlying altered Miocene sands, over an area of the...-
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