-
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
-
RB 79/00058 Reaphook Hill scholzite deposit. MLs 4114, 4368 - C.W. Johnston.
The rare zinc phosphate mineral, scholzite, has been found in gossans developed on Early Cambrian Parachilna Formation siltstone and sandstone near Reaphook Hill in the Flinders Ranges. Other rare phosphate minerals, including tarbuttite,...-
Document
Published: 01 Jan 1979
-
RI 037 Base Metal Occurrences Within Lower Cambrian Sediments Of The Northern Flinders Ranges
There is no abstract created for this record-
Document
-
RB 67/00077 Base metal occurrences within Lower Cambrian sediments of the northern Flinders Ranges.
There is no abstract created for this record-
Document
Published: 12 Feb 1969
-
RB 68/00026 Sedimentary phosphate exploration, Summary Report, Part 1, the Cambrian of the Flinders Ranges.
No sedimentary phosphorate has been found in commercial quantities in outcropping Cambrian rocks of the Flinders Ranges. Two types of minor occurrences were defined: - 1.Those in ferruginous glauconitic limestone (consisting of pelletal apatite)....-
Document
Published: 03 Apr 1969
-
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 71/00203 Geochemical survey of the Mount John-Paralana Fault Zone. Third report.
Seven holes drilled to a maximum depth of 195 ft. (59 m) tested part of the Mt. John Paralana Fault zone for mercury. No anomalous concentrations of mercury were detected. Three holes tested the Parachilna Formation west of the Moro Mine. Anomalous...-
Document
Published: 01 Jan 1973
-
RB 72/00100 Mineral exploration of diapirs in the Adelaide Geosyncline, sixth report, Nantawarrinna Diapir.
There is no abstract created for this record-
Document
Published: 01 Jan 1972
-
RB 76/00117 Turquoise occurrence near Mount John, out of Counties, Flinders Ranges.
There is no abstract created for this record-
Document
Published: 21 Sep 1976
-
RB 2001/00002 Early Cambrian acritarchs, trilobites and archaeocyaths from Yalkalpo 2, eastern Arrowie Basin, South Australia.
Early Cambrian marine sediments in the Arrowie Basin, South Australia, were deposited on a continental margin platform, and have been divided into five unconformity bounded depositional sequences and subsequences, ranging in age from basal Cambrian to...-
Document
Published: 01 Jan 2001
-
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
-
RB 2000/00010 Investigation of the potential for rainwater harvesting at Nepabunna, North Flinders Ranges, South Australia.
The availability of rainwater, and possible harvesting techniques and storage media are investigated. Reasonable amounts of rainfall occur, but falls are interspersed by long droughts. There are problems with silting up of dams, and with protecting...-
Document
Published: 01 Apr 2000
-
Diapir-base metal association in the northern Flinders Ranges.
A number of base metal occurrences in the northern Flinders Ranges, previously classified as syngenetic, diagenetic and epigenetic in nature, appear to have resulted from metalliferous brine-sediment interaction with autochthonous and allochthonous...-
Document
-
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 PARACHILNA (v1): Explanatory Notes PARACHILNA (first edition, 1966)
There is no abstract created for this record-
Document
