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RB 53/00095 Re-appraisal of the Kapunda mine.
Published: 01 Jan 1963 Created: 04 Nov 2024 Revised: 04 Nov 2024
Author: Thomson, B.P.

Bedded sulphide mineralisation has been recognised in the carbonaceous felspathic siltstone host rocks of the Kapunda ore body environment. Evidence for lateral secretion origin for the ore veins is advanced. The new data enable recommendations to...

Bedded sulphide mineralisation has been recognised in the carbonaceous felspathic siltstone host rocks of the Kapunda ore body environment. Evidence for lateral secretion origin for the ore veins is advanced. The new data enable recommendations to be made for further mapping and diamond drilling at the Kapunda Mine.

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About this record

Record No rb5300095
Topic Geoscientific Information
Type of Resource Document
Category Type
Document Type Departmental Publication - Geological Survey Geoscience Publication
Contributor
Sponsor
Tenement
Tenement Holder
Operator
Geological Province
    Mine Name Kapunda Mine
    Stratigraphy
    Commodity copper
    Notes 
    Notes: Published by SADM in: Mining Review, Adelaide. No. 115 (1963); p: 34-37. 61/01793
Geographic Locality: Hd Kapunda
Doc No: RB 53/00095
    Notes: Published by SADM in: Mining Review, Adelaide. No. 115 (1963); p: 34-37. 61/01793
Geographic Locality: Hd Kapunda
Doc No: RB 53/00095
    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/rb5300095
    Citation Thomson, B.P. 1963. RB 53/00095 Re-appraisal of the Kapunda mine. Departmental Publication - Geological Survey Geoscience Publication. Government of South Australia.
    https://pid.sarig.sa.gov.au/document/rb5300095

    Technical information

    Status
    Maintenance and Update Frequency
    Geographic Reference GDA2020 (EPSG:7844)
    Geo bounding box {"type":"Polygon","coordinates":[[[138.5,-34.5],[139,-34.5],[139,-34],[138.5,-34],[138.5,-34.5]]]}
    Purpose 
    
                    
                    
    
                    
                      		
                
    
              
                
                
    
                  
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