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RB 83/00019 1:250 000 Geological Series - Explanatory Notes. DALHOUSIE, South Australia.
The geomorphology of DALHOUSIE broadly consists of stony uplands which include mound springs in the west, and dunefield lowlands in the east on the edge of the Simpson Desert. Strongly folded ?Adelaidean sediments are overlain by a more gently folded...-
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Published: 01 Nov 1984
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Neales River (part of Lake Eyre West Project). Annual reports to licence expiry/full surrender for the period 5/12/2005 to 4/12/2007.
An area of ground located 55 km due west of the northern end of Lake Eyre North was taken up to explore for possible economic uranium mineralisation formed within either Mesozoic to Recent cover rocks or the underlying Proterozoic crystalline...-
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Published: 08 Jan 1908
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Conference poster - [Phanerozoic] Geology of the Peake and Denison Ranges area.
This poster was exhibited to accompany a talk presented by the authors at the 1st Eromanga Basin Symposium, Adelaide, 9-11 November 1982 (the talk abstract is indexed separately).-
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PACE Copper Discovery Drilling (drilling partnerships with DSD and industry): Year 9 partnership DPY9-05 - Mount Sarah Project, Oodnadatta district, Proterozoic basement inferred epithermal/hydrothermal IOCG mineral prospect. Drilling final report.
A small licence area centred approximately 70 km north-northwest of Oodnadatta is being explored for possible economic buried IOCG type mineralisation that may have formed in the wholly concealed, almost unknown basement rocks there. Interest is...-
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Published: 28 Sep 1917
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Geology and petroleum prospects of the Simpson Desert.
Review of virtually all work carried out in area. Discussion of stratigraphy, structure and oil potential of the area. Plans - 1 inch = 1,000 composite section of outcrop of Winnecke divide. 1 inch = 2 miles (h), 5,000 (V) section Decollement folding....-
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Published: 01 Jan 1962
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Data release : Mount Sarah, Alamilda Hill and Todmorden (the Mount Sarah Project). Annual reports and joint annual reports to the successive expiry/full surrender of ELs 6129 and 5634, for the overall period 23/6/2015 to 22/6/2020.
Three adjacent areas located in dissected hilly country 70-90 km to the north-west of Oodnadatta were successsively taken up under licence to cover a significant, 8 mGal regional gravity anomaly which could have potential for IOCG type basement-hosted...-
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Published: 24 Jun 1920
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Block review, basin analysis and hydrocarbon prospectivity of the Pedirka Block in the Pedirka Sector.
The Purni, Peera Peera and Poolowanna Formations were evaluated in terms of depositional and structural basin analysis using the model of Genetic Increments of strata (GIS). Eight reservoir intervals have been identified and the pertinent reservoir...-
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Published: 01 Jan 1986
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1987 Mitchell-PED Seismic Survey, PEL 5 and 6, South Australia. Final geophysical interpretation, acquisition and processing report.
Report describes the outcome of approximately 300 line km of seismic detailing of 2 prospects and 7 strong leads prior to possible Block commitment drilling in 1988-1989. A total of 49 lines derived from 8 Pedirka area seismic surveys, including the...-
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Published: 01 Jan 1990
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Mount Arthur. Progress reports and final report to licence expiry/full surrender, for the period 5/9/1980 to 5/3/1983.
Exploration for possible kimberlite pipes in the Mount Arthur - Mount Toodla area, 30 km east-southeast of Oodnadatta, has included preliminary gravity and ground magnetic surveys, stream sediment sampling, and the drilling of a single diamond cored...-
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Published: 09 Jun 1983
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ExpNotes ABMINGA: Explanatory Notes ABMINGA, SG 53-10.
There is no abstract created for this record.-
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ExpNotes DALHOUSIE: Explanatory Notes DALHOUSIE, SG 53-11.
There is no abstract created for this record.-
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ExpNotes NOOLYEANA: Explanatory Notes NOOLYEANA, SG 53-16.
There is no abstract created for this record.-
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ExpNotes GASON: Explanatory Notes GASON, SG 54-13.
There is no abstract created for this record.-
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ExpNotes WARRINA: Explanatory Notes WARRINA, SH 53-03.
The Peake and Denison Inliers (comprising the Davenport Range, Denison Range and small basement inliers to the east) form the dominant geological structure on WARRINA. The Inliers include outcrops of Palaeoproterozoic metamorphic basement which is...-
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