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RB 80/00033 Walloway Basin seismic and gravity survey.
Created: 06 Nov 2024 Revised: 06 Nov 2024
Author: Finlayson, B.

Results of a seismic refraction and gravity survey conducted in the southern portion of the Walloway Basin suggest that its western margin is influenced by faulting. The survey has also indicated the position of a fault which controls groundwater...

Results of a seismic refraction and gravity survey conducted in the southern portion of the Walloway Basin suggest that its western margin is influenced by faulting. The survey has also indicated the position of a fault which controls groundwater movement within the basin. Five seismic horizons can be recognised within the basin, three of which can be correlated with aquifers. In addition, two types of Precambrian bedrock can be identified beneath the basin fill, which has a maximum thickness of over 300 m.

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About this record

Record No rb8000033
Topic Geoscientific Information
Type of Resource Document
Category Type
Document Type Geophysical Report - Final
Contributor
Sponsor
Tenement
Tenement Holder
Operator
Geological Province Walloway Basin
Mine Name
Stratigraphy
Commodity
    Notes 
    Geographic Locality: Orroroo
Doc No: RB 80/00033
    Geographic Locality: Orroroo
Doc No: RB 80/00033
    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/rb8000033
    Citation Finlayson, B. RB 80/00033 Walloway Basin seismic and gravity survey. Geophysical Report - Final
    https://pid.sarig.sa.gov.au/document/rb8000033

    Technical information

    Status
    Maintenance and Update Frequency
    Geographic Reference GDA2020 (EPSG:7844)
    Geo bounding box {"type":"Polygon","coordinates":[[[138.5,-33],[139,-33],[139,-32.5],[138.5,-32.5],[138.5,-33]]]}
    Purpose 
    
                    
                    
    
                    
                      		
                
    
              
                
                
    
                  
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