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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 WINTINNA: Explanatory Notes WINTINNA, SG 53-14.
A new generation, first edition WINTINNA 1:250 000 scale geological map and explanatory notes have been published. These documents represent the conclusion of the Geological Survey of South Australia's geological mapping program undertaken in the...-
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ExpNotes PANDIE PANDIE: Explanatory Notes PANDIE PANDIE, SG 54-09.
There is no abstract created for this record.-
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RI 026 The Geology and Mineralisation of the Blinman Dome Diapir
There is no abstract created for this record-
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RI 024 Investigation of Lake Eyre Part 1 and Part 2 - 1963
There is no abstract created for this record-
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RB 2004/00001 Palaeochannel studies related to the Harris Greenstone Belt, Gawler Craton, South Australia. Architecture and evolution of the Kingoonya Palaeochannel system.
Exploring the earth resources in the Harris Greenstone Belt (HGB) region is complicated by a regolith cover produced by a long and complex history of landscape evolution. The present surface of the HGB indicates little of the complex palaeochannel...-
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Published: 01 Jun 2004
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Wilcherry Hill. Drilling at the Weednanna Au-Fe deposit, an exploration model for gold deposits formed in the southern Gawler Craton. Collaborative drilling and research final report, Project ADI RD02-265 [Accelerated Discovery Initiative Round 2, 2022].
Between 8 August and 6 October 2021, six inclined, rotary mud precollared diamond cored holes (21WDDH001 to 006) totalling 1560.6 m were drilled at the Weednanna gold and iron deposit located ~40 km north of Kimba on northern Eyre Peninsula, as part...-
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Bull 052 Stratigraphy and Tectonics of the Worumba Anticline and Associated Intrusive Breccias
The Worumba Anticline contains in its core a complex of intensely deformed and brecciated Callanna and Burra Group sediments and volcanics, surrounded by a less deformed rim sequence of unconformably overlying Umberatana Group sediments. The...-
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RB 2018/00038 Gawler Craton Airborne Geophysical Survey Region 3B, Torrens – Enhanced geophysical imagery and magnetic source depth models
This report presents the results of a study jointly conducted by the Geological Survey of South Australia and CSIRO Mineral Resources which aimed to enhance the expression of geological structure in geophysical images and to derive depth to magnetic...-
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Published: 01 Dec 2018
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RB 2018/00037 Gawler Craton Airborne Geophysical Survey Region 3A, Andamooka – Enhanced geophysical imagery and magnetic source depth models
This report presents the results of a study jointly conducted by the Geological Survey of South Australia and CSIRO Mineral Resources which aimed to enhance the expression of geological structure in geophysical images and to derive depth to magnetic...-
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Published: 01 Dec 2018
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RB 2018/00026 Sedimentology of the late Palaeozoic Cape Jervis Formation, Troubridge Basin, South Australia.
The late Palaeozoic Cape Jervis Formation of the Troubridge Basin in southern South Australia provides a sedimentological record of the glacial environment during the Permo-Carboniferous glaciation. The sedimentary sequence is divided into five...-
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Published: 01 Nov 2018
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RI 057 Cambrian Sediment-hosted Exhalative Base Metal Mineralisation, Kanmantoo Trough, South Australia
A deformed and metamorphosed succession of sandstone, greywacke, siltstone and shale which accumulated in the Early Cambrian Kanmantoo Trough hosts a number of exhalative base and precious metal deposits. This sequence is apparently devoid of...-
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RI 051 Andamooka Opal Fields The Geology of the Precious Stones Field and The Results of the Subsidised Mining Program
Since discovery of the opal field in 1930, Andamooka, 640 km by road north of Adelaide, has been a major world producer of precious opal. All workable opal at Andamooka has been found in the Marree Formation, a sequence of marine sediments of...-
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RI 041 Hydrocarbon Potential of Western Murray Basin and Infrabasins
The Murray Basin is a shallow, saucer-shaped Tertiary basin covering an area of 120 700 square miles extending from the western foot of the Snowy Mountains in New South Wales and Victoria to the Mount Lofty Ranges in South Australia. Geophysical work...-
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RI 030 The Construction Sand Industry in the Adelaide Metropolitan Area
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Bull 013 Pigment Minerals in South Australia
During the past twenty years attention has been directed to the natural resources of the State in pigment materials, and a considerable body of information, based 011 official reports, has been accumulated, which is now collected into this Bulletin,...-
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Bull 012 Clay and Cement in South Australia
In South Australia the scarcity of easily obtainable timber, as compared to the other Australian States, and especially the absence of softwoods, led to the utilization of stone and clay. Stone is very extensively used for building, both in its...-
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RI 038 Tertiary Stratigraphy of Three Deep Bores in the Waikerie Area of the Murray Basin
Three observation bores were drilled within 1.5km of each other approximately 4km south-west from Waikerie. Depth ranged from 235 to 329m, substantially deeper than all othe bores in the area, and all Tertiary epochs are represented. The stratigraphic...-
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RB 2002/00007 The Palaeo-Mesoproterozoic geology of northern Yorke Peninsula, South Australia. Hiltaba Suite - related alteration and mineralisation of the Moonta - Wallaroo Cu-Au district (Resources '96 Convention, Adelaide, geological field excursion
Returns from copper and gold won from the Moonta-Wallaroo district supported the South Australian economy from 1860-1920. During those 60 years some 355,000 t of copper and 2 t of gold were extracted from the twin mining fields of Wallaroo and Moonta:...-
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Published: 01 Nov 1996
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RB 2002/00019 16th Australian Geological Convention, Adelaide, South Australia, 1-5 July 2002 - Pre-conference Excursion A4 locality guide. Geology and tectonic evolution of the Delamerian Fold Belt in southern South Australia and western Victoria.
Adelaide lies towards the western margin of the Delamerian Fold Belt which extends across strike as far east as the Glenelg Province in western Victoria. Outcrop across this belt is very incomplete as most of the region of the Murray Basin is covered...-
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Published: 01 Jun 2002