-
RB 43/00030 Report on foundation testing, Government Sawmill, Mount Gambier, secn 1235 Hd Gambier.
During construction of the green mill at Mount Gambier Government sawmill, cavities were found in excavations for a gangsaw in the Gambier Limestone. Diamond drilling showed the main cavity to be funnel-shaped and not a cavern top, but revealed minor...-
Document
Published: 01 Jan 1956
-
RB 42/00039 Report on prospects of underground drainage of a swamp, block 54 Hd Naracoorte - G. Newland.
There is no abstract created for this record-
Document
Published: 01 Jan 1956
-
RB 44/00076 Report on groundwater prospects, Section 84, Hundred of Laffer.
There is no abstract created for this record-
Document
Published: 24 Apr 1957
-
RB 43/00062 Copper prospect, Mutooroo Station.
Copper carbonates are found irregularly dispersed within two types of quartz reef occurring in sheared Adelaide System quartzites and slates, 26 miles east south-east of Radium Hill and 4 miles south- southwest of Mutooroo Homestead. Mining there was...-
Document
Published: 25 Sep 1956
-
RB 44/00028 Second report on foundation testing, Government Sawmill, Mount Gambier, secn 1235 Hd Gambier, Co. Grey.
Following the discovery, drilling and grouting of a large cavity in the proposed foundation area for the green milling section of the Mt Gambier Government sawmill, a second large cavity was found in the same area. A further 29 diamond drill holes...-
Document
Published: 01 Jan 1957
-
RB 42/00078 Proposed salt industry, Wallaroo.
In response to a request from the Corporation of the town of Wallaroo an inspection was made of swamp areas adjacent to the town boundaries for the purpose of accessing the salt producing potential of these areas. The request for this inspection arose...-
Document
Published: 01 Jan 1957
-
RB 44/00068A Report on groundwater prospects, Section 84, Hundred of Laffer.
There is no abstract created for this record-
Document
Published: 24 Apr 1957
-
RB 47/00010 Report on the East Boolcunda Triassic basin.
The East Boolcunda Basin was examined in order to map the Triassic rocks in detail and to assess their coal-bearing potentiality. It was found that these rocks conform to a true basin structure, similar in most respects to the Leigh Creek and...-
Document
Published: 04 Jul 1958
-
RB 48/00083 Rock specimens with mollusca from the Musa River area, Papua.
4 specimens from the Domara River Beds, Papua, submitted by Bureau of Mineral Resources contained fresh water gastropoda referable to Cipangopaludina and Melanoides. The rocks are regarded as of non-marine origin and probable Pleistocene age.-
Document
Published: 01 Jan 1959
-
RB 77/00011 Northern Adelaide Plains surface water assessment 1971-1975.
Flow measurements on the Gawler and Little Para Rivers since 1971 indicate a substantial loss in surface flow as the rivers cross the plains from Gawler and Carisbrooke Park respectively. These losses are due to recharge of the aquifer and...-
Document
Published: 01 Jan 1977
-
RB 77/00117 Investigation of the heavy mineral sands along the coast of Eyre Peninsula.
There is no abstract created for this record-
Document
Published: 01 Jan 1977
-
RB 78/00116 Mount Gambier Mulga St Primary School site gravity survey.
A proposed Primary School will be constructed on thinly covered limestone in an area near caves and sinkholes. To avoid siting buildings on collapsible areas, a 601 station gravity survey was conducted on a 5 m grid. No near-surface voids were...-
Document
Published: 01 Jan 1978
-
RB 79/00129 Explanatory Notes for the FROME 1:250 000 geological map sheet SH54-10 international index.
The FROME 1: 250 000 geological sheet is located between latitudes 30° S and 31° S and longitudes 139°30' E and 141° E and covers most of the area between the northern Flinders Ranges and the New South Wales border. Its southern and northern limits...-
Document
Published: 01 Jan 1980
-
RB 82/00054 Geological notes on the liquids pipeline trench south of Moomba South Australia.
The trench from Moomba gasfield was examined to 20 km south. The sediments were alluvial quartz sand occupying a flood plain between sand ridges, and may be of Pleistocene to Holocene age, possibly equivalent to Tingana Clay. A carbonate palaeosol has...-
Document
Published: 01 Jul 1982
-
RB 83/00009 Magnetic fraction of a sand near Moomba.
The heavy mineral fraction of an alluvial sand south of Moomba contains fine black magnetic grains. X-ray diffraction and electron probe analyses show that the magnetic grains have a hexagonal crystal structure intermediate between that of hematite...-
Document
Published: 01 Jan 1983
-
RB 83/00077 Petrography of forty-two specimens from the Wangianna sheet.
Forty-two thin sections collected from the Skillogalee Dolomite are representative of carbonate and non-carbonate facies, and include shales, siltstones, sandstones and conglomerates. Many of the specimens are partly or wholly stromatolitic: two...-
Document
Published: 01 Oct 1983
-
RB 84/00010 Torrens Island sand resource, secn 453, Hd Port Adelaide, Co. Adelaide.
The deposit is worked for filling sand, but is suitable for replenishment of beaches, and with beneficiation, for glass and foundry. Reserves, based on 110 auger holes, are 835 000 tonnes (indicated) and 270 000 tonnes (inferred).-
Document
Published: 01 Feb 1984
-
RB 84/00058 Progress report: CURDIMURKA 1:250 000 geological map - Cainozoic geology.
Two sandstone sequences, one un-named and one equivalent to the Watchie Sandstone, have been recognized on CURDIMURKA. These sandstone sequences occur beneath the Etadunna Formation. Both are believed to be equivalent to the Eyre Formation. The...-
Document
Published: 01 Sep 1984
-
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...-
Document
Published: 01 Nov 1984
-
RB 83/00022 Pata Limestone whale bone matrix, Sunlands, Murray Basin.
The benthonic foraminifera `Heterolepa victoriensis indicates unit is Pata Limestone of early Middle Miocene age.-
Document
Published: 01 Jan 1983