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RB 82/00054 Geological notes on the liquids pipeline trench south of Moomba South Australia.
Published: 01 Jul 1982 Created: 06 Nov 2024 Revised: 06 Nov 2024
Author: Forbes, B.G.;Krieg, G.W.

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...

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 developed within the sediments.

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About this record

Record No rb8200054
Topic Geoscientific Information
Type of Resource Document
Category Type
Document Type Departmental Publication - Engineering Geology Publication
Contributor
Sponsor
Tenement
Tenement Holder
Operator
Geological Province
    Mine Name
    Stratigraphy
    Commodity
      Notes 
      Geographic Locality: Moomba
Doc No: RB 82/00054
      Geographic Locality: Moomba
Doc No: RB 82/00054
      Language English
      Metadata Standard ISO 19115-3

      Citations

      Use constraints License
      License Creative Commons Attribution 4.0
      Persistent identifier https://pid.sarig.sa.gov.au/document/rb8200054
      Citation Forbes, B.G.;Krieg, G.W. 1982. RB 82/00054 Geological notes on the liquids pipeline trench south of Moomba South Australia. Departmental Publication - Engineering Geology Publication. Government of South Australia.
      https://pid.sarig.sa.gov.au/document/rb8200054

      Technical information

      Status
      Maintenance and Update Frequency
      Geographic Reference GDA2020 (EPSG:7844)
      Geo bounding box {"type":"Polygon","coordinates":[[[140,-28.5],[140.5,-28.5],[140.5,-28],[140,-28],[140,-28.5]]]}
      Purpose 
      
                    
                    
      
                    
                        		
                
      
              
                
                
      
                  
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