-
RB 58/00158 Lower Cambrian stratigraphy of the Flinders Ranges.
The distribution and relationships of Lower Cambrian units in the Flinders Ranges are illustrated by a panel diagram and sketch maps. A new rock name, Hawker Group, is introduced for six formations of Lower Cambrian age which represent a phase of...-
Document
Published: 01 Jan 1964
-
Ediacara Range. Annual reports and final report to licence expiry/full surrender, for the period 5/6/1997 to 4/6/1999.
No significant gold or base metal values were returned from geochemical sampling of quartz and barite veins in the vicinity of the Ediacara Fault, 40 km north-west of Parachilna. Imaging of aeromagnetic data purchased as infill coverage to a 1999...-
Document
-
Frome Downs Homestead. Progress and technical reports to licence expiry/renewal, for the period 1/1/1969 to 31/12/1970.
Reconnaissance shallow stratigraphic drilling with subsequent borehole geophysical electric and radioactivity logging in the south-western Frome Embayment (21 rotary mud partly cored holes, total 8841 feet), over areas lying adjacent to outcropping...-
Document
Published: 31 Dec 1970
-
Reaphook Hill (part of the Flinders Ranges Project). Sixth partial surrender report, for the period 4/8/1997 to 29/8/2019.
The northern portion of EL 6132, comprising ~0.59% of its former area, was relinquished by the JV partners on 18/7/2019. The only work performed within the now relinquished ground has consisted of reconnaissance + infill surface geochemical sampling...-
Document
Published: 10 Sep 1919
-
PEL 47. Progress and technical reports for the period June 1990 to March 1993.
Anzoil NL carried out geological and geophysical studies on previous exploration data, but was unsuccessful in attracting farmin partners either locally or overseas. The licence area was reduced to ease the work commitment, by partial relinquishment...-
Document
Published: 31 Mar 1993
-
Data release [made at SA Director of Mines' discretion] : Reaphook Hill (formerly part of the Flinders Ranges Project). Licence-specific annual reports for the period 27/9/2015 to 26/9/2018.
A small area centred ~110 km south-east of Copley is being explored for possible buried economic Beltana style zinc silicate mineralisation, as well as for possible epigenetic hydrothermal lead-zinc sulphide and copper mineralisation. During...-
Document
Published: 26 Nov 1918
-
Source rock maturity study and petroleum geochemistry of the Arrowie Basin.
This section of the study was based on source rock analyses performed on 75 outcrop and shallow drill core samples from 25 localities, plus other new data derived from Cambrian sediments intersected in the deep petroleum exploration wells Moorowie 1,...-
Document
Published: 13 Jan 1986
-
1981 and 1982 seismic surveys, Wertaloona and Christmas Creek-ARR, final report.
Wertaloona Seismic Survey - AIM:The 1981 Wertaloona Seismic Survey programme was designed by the PELs 5 and 6 Arrowie Block partners to provide the first high quality, multifold seismic reflection data in the area of likely preserved thick Cambrian...-
Document
-
Arrowie Block acreage assessment.
During the period January 1946-December 1985 under review, the following petroleum exploration work was carried out over the Arrowie Block: 6 gravity, 2 aeromagnetic and 10 seismic surveys (total seismic coverage 2781 line km), plus 4 wells, all dry....-
Document
-
RB 71/00035 PARACHILNA, South Australia, sheet SH54-13 International Index.
The Parachilna 1:250 000 map area is about 250 road miles north of Adelaide, South Australia, and includes the eastern shore of Lake Torrens, the central Flinders Ranges and part of the Lake Frome Plains. The ranges are composed of folded Adelaidean...-
Document
Published: 01 Jan 1972
-
RB 71/00178 Explanatory Notes for the COPLEY 1:250 000 geological map.
The COPLEY 1:250 000 map area includes the northern Flinders Ranges and the southern part of the Willouran Ranges. It is bounded to the west by the Lake Torrens Sunkland and, to the east, by the Lake Frome Plains. A thick sequence of older Precambrian...-
Document
Published: 08 Nov 1971
-
RB 2002/00024 Sequence analysis and petroleum potential in the Arrowie Basin, South Australia.
Cambrian sediments in the Arrowie Basin were deposited on a rifted continental margin. Four distinct depositional regimes, ranging from a western, tectonically stable shelf, through platform-ramp to eastern slope and trough-synclines, can be...-
Document
Published: 01 Feb 2003
-
Teatree Well. Progress and final reports to licence expiry/full surrender for the period 5/1/1984 to 4/1/1986.
Exploration for possible fault-related epigenetic lead-zinc deposits formed in calcareous rocks outcropping along the Mount John - Arrowie fault system, to the south-east of the Moro mine, has included extensive stream sediment and rock chip sampling...-
Document
-
Mount Lyall. Progress and final reports to licence expiry/renewal for the period 1/5/1969 to 24/3/1971.
The Third Plain zinc silicate (willemite) deposit, located 14 miles south-east of Blinman, has been newly assessed by North Flinders Mines for its economic potential. Originally discovered by Kennecott Explorations in late 1966, and evaluated by them...-
Document
-
Curnamona Homestead. Progress and technical reports to licence expiry/renewal, for the period 1/1/1969 to 31/12/1970.
Reconnaissance shallow stratigraphic drilling with subsequent borehole geophysical electric and radioactivity logging in the south-western Frome Embayment (21 rotary mud partly cored holes, total 8841 feet), over areas lying adjacent to outcropping...-
Document
Published: 31 Dec 1970
-
RB 2002/00033 Correlation within Early Palaeozoic basins of eastern South Australia.
The great majority of lower Palaeozoic rocks in the Stansbury, Arrowie and Warburton Basins are of Cambrian age, although a few Early Ordovician fossils have been reported from drillholes in the sub-surface Warburton Basin. The Cambrian is the only...-
Document
Published: 01 Dec 2002
-
ExpNotes COPLEY: Explanatory Notes COPLEY
There is no abstract created for this record-
Document
-
ExpNotes PARACHILNA (v2): Explanatory Notes PARACHILNA (second edition, 1999)
The PARACHILNA map area (31 to 32°S, 138 to 139.5°E) occupies the central Flinders Ranges which are made up of folded, mostly marine sedimentary Neoproterozoic and Cambrian rocks of the Adelaide Geosyncline, and adjoining plains underlain by Cainozoic...-
Document
-
ExpNotes PARACHILNA (v1): Explanatory Notes PARACHILNA (first edition, 1966)
There is no abstract created for this record-
Document