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RB 51/00009 Geophysical investigation of the Blinman Dome.
Published: 01 Jan 1961 Created: 04 Nov 2024 Revised: 04 Nov 2024
Author: Mumme, I.A.

The results of this investigation show a small gravity "low" over the structure suggesting that the rock formations beneath the central portion of the Dome are less dense than those comprising the surrounding area. No significant magnetic...

The results of this investigation show a small gravity "low" over the structure suggesting that the rock formations beneath the central portion of the Dome are less dense than those comprising the surrounding area. No significant magnetic variations were observed. It-is concluded that the results are broadly in agreement with the structure being of diapiric origin, as suggested by geological mapping.

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About this record

Record No rb5100009
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
    Commodity
      Notes 
      Notes: 59/01625
Geographic Locality: Blinman Dome
Doc No: RB 51/00009 p: na
      Notes: 59/01625
Geographic Locality: Blinman Dome
Doc No: RB 51/00009 p: na
      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/rb5100009
      Citation Mumme, I.A. 1961. RB 51/00009 Geophysical investigation of the Blinman Dome. Geophysical Report - Final
      https://pid.sarig.sa.gov.au/document/rb5100009

      Technical information

      Status
      Maintenance and Update Frequency
      Geographic Reference GDA2020 (EPSG:7844)
      Geo bounding box {"type":"Polygon","coordinates":[[[138.5,-31.5],[139,-31.5],[139,-31],[138.5,-31],[138.5,-31.5]]]}
      Purpose 
      
                    
                    
      
                    
                        		
                
      
              
                
                
      
                  
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