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RB 73/00030 Seismic refraction survey at Hindmarsh Valley.
Published: 07 Feb 1973 Created: 06 Nov 2024 Revised: 06 Nov 2024
Author: Nelson, R.G.

Seismic refraction traverses along the right abutment ridge of a proposed dam in Hindmarsh Valley were used to predict depth to Cambrian bedrock. The results indicated that the bedrock core of the abutment ridge falls in some places below the full...

Seismic refraction traverses along the right abutment ridge of a proposed dam in Hindmarsh Valley were used to predict depth to Cambrian bedrock. The results indicated that the bedrock core of the abutment ridge falls in some places below the full storage level of the dam. A cable-tool hole, drilled at a critical site on the ridge, confirmed the result of the seismic traverse at this point.

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About this record

Record No rb7300030
Topic Geoscientific Information
Type of Resource Document
Category Type
Document Type Geophysical Report - Final
Contributor
Sponsor
Tenement
Tenement Holder
Operator
Geological Province
    Mine Name
    Stratigraphy Kanmantoo Group
    Commodity
      Notes 
      Geographic Locality: Hindmarsh
Doc No: RB 73/00030
      Geographic Locality: Hindmarsh
Doc No: RB 73/00030
      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/rb7300030
      Citation Nelson, R.G. 1973. RB 73/00030 Seismic refraction survey at Hindmarsh Valley. Geophysical Report - Final
      https://pid.sarig.sa.gov.au/document/rb7300030

      Technical information

      Status
      Maintenance and Update Frequency
      Geographic Reference GDA2020 (EPSG:7844)
      Geo bounding box {"type":"Polygon","coordinates":[[[138.5,-35.5],[139,-35.5],[139,-35],[138.5,-35],[138.5,-35.5]]]}
      Purpose 
      
                    
                    
      
                    
                        		
                
      
              
                
                
      
                  
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