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EL 6809 Annual Technical Report to period ending 02/08/2023
This is the first annual report for activities on EL 6809 Tourmaline Hill. The license is located approximately 20 km northwest of Arkaroola Village in the north Flinders Ranges, and covers an area of 741 sq km. The area was considered prospective for...-
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Published: 28 Sep 2023
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EL 6710, EL 6711, EL 6720, EL 6735, EL 6738 - Innamincka area. Final technical reports for the period 01/04/2022 to surrender 08/06/2023.
A group of 5 exploration licences EL’s 6710, 6711, 6720, 6735 and 6738, situated in the north-eastern corner of South Australia within the Cooper Basin, covering a cumulative area of 4434 square km were being explored for their potential for lithium...-
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Published: 03 Aug 1923
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RB 2011/00003 PACE Geochronology: Results of collaborative geochronology projects [performed during] 2009-2010.
This report book presents the results of seven geochronology research projects completed during 2009 and 2010 as a new part of the ongoing PACE Initiative geoscientific data gathering activity underwritten by the South Australian Government. It has...-
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Published: 01 Apr 2011
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RB 2015/00003 PACE Geochronology: Results of collaborative geochronology projects, 2013–2015.
The PACE Geochronology program fosters collaboration on projects of geological and metallogenic significance with focus on dating rocks and minerals from samples suggested by companies through a competitive proposal-based selection process. Successful...-
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Published: 01 Aug 2017
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RB 2018/00010 Characterising and mapping alteration in the Punt Hill region - a data integration project.
South Australia’s Olympic Cu-Au Province hosts some of the world’s great iron oxide copper gold (IOCG) deposits, such as Olympic Dam, Prominent Hill and Carrapateena. The same causative thermal event resulted in variants of this deposit class being...-
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Published: 01 May 2018
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RB 55/00124; Amdel 00205 Phosphate deposits, Kapunda. Production of phosphoric acid.
At least 90% of the phosphate was leached with either nitric, hydrochloric or sulphuric acids. Products unsuitable for the surface preparation of steel. The most promising outlet would be for upgrading the P2O5 content of super phosphate fertilizer.-
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Published: 01 Oct 1962
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Bull 055 A geochronological framework for the Gawler Craton, South Australia
This bulletin contains geochronological data and interpretations from the Gawler Craton of South Australia that have been completed by Mark Fanning of The Australian National University, by Geological Survey of South Australia personnel, and by...-
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EL 6920 Partial Surrender Report to period ending 15/08/2024
This report represents a partial surrender of EL 6920 "The Tapanappa Project" and covers work completed in the reporting period to 15th August 2024. The Tapanappa Project area is located approximately 60 km south of Adelaide on the Fleurieu Peninsula...-
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Published: 12 Oct 2024
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EL 6437 Annual Technical Report to period ending 24/11/2021
The Torrens Project is located in the Flinders Ranges of South Australia, approximately 140 km north-west of Port Augusta and 30 km north of Hawker. It sits along the eastern margin of the Gawler Craton at the intersection of the G2 & G8...-
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Published: 16 Jan 2022
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RB 2023/00038 Quantitative Mineral Resource Assessment of undiscovered sedimentary-hosted copper in South Australia.
Sedimentary-hosted copper deposits are the second most important source of copper in the world with most South Australian sediment-hosted copper occurrences located within the Adelaide Rift Complex, Torrens Hinge Zone and Stuart Shelf. In response to...-
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Published: 01 Sep 2023
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RB 06/00285 Report on asbestos, section 13 Hundred of Miltalie.
A newly found, up to 2 inch wide vein of asbestos occurring within a magnesian marble bed in the Mount Olinthus district was inspected and qualitatively assessed from a single shallow trench exposure.-
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Published: 15 Apr 1919
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PACE Theme 2 (drilling partnerships with PIRSA and industry): Year 6 partnership DPY6-63 - Gawler Iron Project, Mount Christie district - Archaean BIF hosted stratabound iron ore prospects. Drilling project final report.
The Gawler Iron Project is situated approximately 25 km north of the Trans-Australian Railway and 200 km south-west of Coober Pedy, along the western margin of the Gawler Craton in South Australia. The project area formerly had not been systematically...-
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Published: 30 Jan 1912
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South Australian Mineralogical Data package - VNIR_GROUP_OXIDE_uTSAV.
This data package contains three sets of GOCAD 3D objects. Data assembled in the sets comprise complete "Oxide" minerals spectral logs determined using visible and near visible wavelength range infrared absorption, for all drillholes that have been...-
Dataset
Published: 25 Nov 1916
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ExpNotes MAITLAND: Explanatory Notes MAITLAND, SI 53-12.
The MAITLAND Special 1:250,000 scale geological map covers the greater part of South Australia's Yorke Peninsula. The rocks in the map area comprise deformed Palaeoproterozoic and early Mesoproterozoic basement of the south-eastern Gawler Craton, and...-
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Published: 01 Jul 2006
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ExpNotes LINCOLN: Explanatory Notes LINCOLN, SI 53-11.
The LINCOLN 1:250,000 scale regional geological map area covers southern Eyre Peninsula and includes numerous islands lying off its eastern, southern and western coasts. The region encompasses a complex geological history and contains a variety of...-
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ExpNotes GILES: Explanatory Notes GILES, SH 53-01.
Concealed basement on GILES comprises ?Archaean to Palaeoproterozoic metamorphic rocks belonging to the Nawa Subdomain of the Gawler Craton. These are intruded by Mesoproterozoic Hiltaba Suite granitic bodies and Mesoproterozoic or Neoproterozoic...-
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ExpNotes YARDEA: Explanatory Notes YARDEA, SI 53-03.
The YARDEA 1:250,000 scale regional geological map area straddles the southern margin of the Gawler Ranges on northern Eyre Peninsula. The only major township within the area is Minnipa, with Kimba and Wudinna both located immediately south of the...-
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ExpNotes PARACHILNA (v2): Explanatory Notes PARACHILNA (second edition, 1999), SH 54-13.
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...-
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