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RB 70/00118 Murray Bridge to Onkaparinga pipeline, summit storage, Mount Barker junction. secns 4262, 4263, 5214 Hd Onkaparinga, and secn 4412 Hd Macclesfield. Geological investigations, progress report no. 1 - EWS Department.
Tributary of the Onkaparinga River is to be dammed by an earth - and - rock embankment. Includes data for design of stable batters, prediction of excavation conditions, foundation conditions for dam embankment, spillway, outlet conduit and assessment...-
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Published: 10 Aug 1970
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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
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RB 72/00161 Explanatory Notes for the LINDSAY 1:250 000 geological map.
The LINDSAY 1 :250 000 sheet area occupies parts of the southern Musgrave Block and the northern Officer Basin, in the North West Province of South Australia. It is entirely contained by the Great Victoria Desert. The oldest rocks are gneisses of...-
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Published: 21 Aug 1972
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RB 73/00156 Groundwater survey, Hundred Para Wirra, part section 134 - J.M. Keen.
There is no abstract created for this record-
Document
Published: 26 Jun 1973
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RB 72/00082 Report on Investigations of Mineral Claims 7310 and 7311 Section 1G, Hundred Bright - Burra Florienton (inspected 8/5/1972).
The two mineral claims no's. 7310 and 7311 lie 6 miles miles (9.6 km) northeast of Robertstown in the Hundred of Bright, Section 1G, some 86 miles (138 km) by road northeast of Adelaide (Fig. 1). The investigation was undertaken at the request of the...-
Document
Published: 08 May 1977
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RB 72/00080 Investigation of clay (weathered shale) occurrences in the Birdwood area.
White weathered shale in the Birdwood area appears to be associated with north-south trending quartzite ridges. Scout drilling is recommended between quartzite ridges south of the pit in Section 6397, Hundred of Talunga.-
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Published: 01 Jan 1972
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RB 72/00094 Proterozoic stromatolites - Successions, correlations and problems.
Stromatolites afford a means of stratigraphic subdivision and correlation in Precambrian sequences which, contain few or no other fossils. Detailed field and laboratory studies are necessary in order to classify stromatolites. Determination of the...-
Document
Published: 23 May 1972
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RB 73/00004 Investigation of the Anabama copper and molybdenum prospect, Olary Wadnaminga.
Stream sediment sampling, induced polarization surveys and a 44 drill hole rotary drilling program were undertaken over the Anabama Granite. The granite was found to be unmineralized except for greisened portions containing anomalous copper and...-
Document
Published: 01 Jan 1973
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RB 70/00037 Progress of mapping in the Olary region.
Adelaidean and younger rocks of the Yunta, Winnininnie, Oakvale, Mutooroo, Ballara, Wadnaminga, Olary and Manunda one mile areas are summarised.-
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Published: 25 Feb 1970
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RB 62/00025 Progress of mapping on the ORROROO 1:250 000 sheet area.
Up to 30,000 feet of strata referred to the Adelaide System outcrop over the ORROROO 1:250,000 mapsheet area in the upper Mid-North of the State. The majority of the area has been geologically mapped, and only some localities in the south-west require...-
Document
Published: 24 Jan 1966
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RB 61/00130 Preliminary report on the Precambrian stratigraphy of the Carrieton 1-mile sheet.
The Carrieton 1:63, 360 map area lies about 200 miles north of Adelaide, South Australia. It contains folded rocks of the Burra, Umberatana and Wilpena Groups of the Adelaide System, of Upper Precambrian age; total thickness of these rocks exceeds...-
Document
Published: 01 Jan 1965
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RB 62/00034 Geology of the Spalding Willouran Inlier.
The Spalding inlier is a lens-shaped area of tightly-folded Willouran rocks of the Adelaide System (Upper Precambrian), extending north-south for about 10 miles; it is about 100 miles north of Adelaide. The rim of the inlier is marked in most places...-
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Published: 09 Feb 1966
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RB 63/00082 Report on dolomite deposit near Williamstown, secn 309 Hd Barossa - A.H. London.
The country rocks consist of Burra Group (Torrensian) formations which have been metamorphosed to dolomite, marble and quartz-mica-schist. The dolomite appears to be of poor quality, easily weathered and it is contaminated with pyrite which has been...-
Document
Published: 01 Jan 1966
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RB 73/00219 Little Para Dam proposed spillway alignment. Report on geological investigations - EWS Department.
There is no abstract created for this record-
Document
Published: 01 Jan 1973
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RB 74/00203 (Results of an) Experimental resistivity survey over quartz reefs in the Wadnaminga Goldfield (on Wadnaminga 1:63,360 mapsheet area).
An experimental test resistivity profiling method, using a two electrode array, was used to determine the resistivity characteristics of thin quartz reefs in the Wadnaminga Goldfield area. The results were negative, but demonstrated the usefulness of...-
Document
Published: 17 Oct 1974
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RB 73/00232 Little Para Dam, geological investigations progress report no. 4, Hundreds of Munno Para and Yatala.
Geological investigations for a 53 m high dam on the Little Para River 22 km north of Adelaide have shown that the site is formed by Proterozoic quartzites, slates and shaley dolomites. The metasediments dip uniformly 25° east and at the dam site a...-
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Published: 01 Jan 1973
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RB 73/00236 Fluorite deposit, Mutooroo - Mrs T.V. Alfonzi.
There is no abstract created for this record-
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Published: 01 Jan 1973
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RB 73/00296 Sillimanite, kyanite, andalusite, SA. In: Knight, C.L. (Ed.) - Economic geology of Australia and Papua New Guinea. 4, Industrial minerals and rocks.
Sillimanite, andalusite and kyanite are three minerals with the same chemical composition (Al2SiO5) but with distinctive crystal structure and heating properties. All eventually convert to mullite at high temperatures. Sillimanite is the most...-
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Published: 01 Jan 1976
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RB 73/00310 Little Para Dam detailed geological mapping of the grout cap alignment, Hds Yatala and Munno Para - EWS Department.
The grout cap will traverse both hillsides between the river level and EL 153 and is to be 4m wide. Rock quality to be expected along both sides of the alignment is shown on a large scale geological map together with a tabulation of recommended...-
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Published: 01 Jan 1974
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RB 76/00057 Report on Deloraine mine.
There is no abstract created for this record-
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Published: 01 Jan 1978
