-
Northern Flinders Ranges, part COPLEY [mapsheet area] regional geology 3D Model (3D pdf version 1)
The northern to central Flinders Ranges area comprise uplifted and eroded remnants of openly folded sedimentary rocks that were deposited in an intra-continental arm of the Neoproterozoic to Early Cambrian Adelaide Geosyncline. Deposition was...-
Model
- ZIP,
-
Central Flinders Ranges, part PARACHILNA [mapsheet area] regional geology 3D Model (GOCAD version 1).
Upper crustal strata forming the northern to central Flinders Ranges area comprise uplifted and eroded remnants of openly folded sedimentary rocks that were deposited in an intra-continental arm of the Neoproterozoic to Early Cambrian Adelaide...-
Model
- ZIP,
-
Northern Flinders Ranges, part COPLEY [mapsheet area] regional geology 3D Model (GOCAD version 1).
The northern to central Flinders Ranges area comprise uplifted and eroded remnants of openly folded sedimentary rocks that were deposited in an intra-continental arm of the Neoproterozoic to Early Cambrian Adelaide Geosyncline. Deposition was...-
Model
- ZIP,
-
3D cover map for the eastern Gawler Craton IOCG province (including Emmie Bluff area detailed map). (3D pdf version).
The eastern Gawler Craton hosts the giant Olympic Dam iron oxide - associated copper-gold (IOCG) deposit, as well as several other world class IOCG deposits (i.e. Prominent Hill and Carrapateena). The region is covered by a thick sequence of...-
Model
- ZIP,
-
3D cover map for the eastern Gawler Craton IOCG province (including Emmie Bluff area detailed map). (GOCAD version).
The eastern Gawler Craton hosts the giant Olympic Dam iron oxide - associated copper-gold (IOCG) deposit, as well as several other world class IOCG deposits (i.e. Prominent Hill and Carrapateena). The region is covered by a thick sequence of...-
Model
- PDF,
- ZIP
-
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
-
RB 2017/00048 Geological Field Excursion Guide from Arkaroola to Sillers Lookout.
The 4WD vehicle journey of ~22 km length from Arkaroola Village to Sillers Lookout, along the world famous Ridgetop Track, presents the opportunity to view some amazing landscapes and associated geological features that the Arkaroola Pastoral Station...-
Document
Published: 01 Jul 2017
-
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...-
Document
Published: 01 Apr 2011
-
ExpNotes CALLABONNA: Explanatory Notes CALLABONNA, SH 54-06.
There is no abstract created for this record.-
Document
-
ExpNotes MARREE: Explanatory Notes MARREE, SH 54-05.
A new generation, second edition MARREE 1:250 000 scale geological map and its explanatory notes have been published. These documents represent the conclusion of the Geological Survey of South Australia's latest geological mapping program (1993 to...-
Document
-
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...-
Document