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RB 84/00034 Petrography of three rocks from Curdimurka.
Published: 01 May 1984 Created: 06 Nov 2024 Revised: 06 Nov 2024
Author: Farrand, M.G.

Sandstone cemented by limonite near Cockatoo Bore represents the uppermost unit of Algebuckina Sandstone (Late Jurassic or Early Cretaceous). 2 sandstones replaced by haematite from Finniss Springs station represent either Cadna-owie Formation or...

Sandstone cemented by limonite near Cockatoo Bore represents the uppermost unit of Algebuckina Sandstone (Late Jurassic or Early Cretaceous). 2 sandstones replaced by haematite from Finniss Springs station represent either Cadna-owie Formation or basal Bulldog Shale (Early Cretaceous). All the specimens were iron enriched, probably in the same iron mineralization process.

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Record No rb8400034
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 Eromanga Basin
Mine Name
Stratigraphy
Commodity
    Notes 
    Geographic Locality: Curdimurka
Doc No: RB 84/00034
    Geographic Locality: Curdimurka
Doc No: RB 84/00034
    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/rb8400034
    Citation Farrand, M.G. 1984. RB 84/00034 Petrography of three rocks from Curdimurka. Departmental Publication - Geological Survey Geoscience Publication. Government of South Australia.
    https://pid.sarig.sa.gov.au/document/rb8400034

    Technical information

    Status
    Maintenance and Update Frequency
    Geographic Reference GDA2020 (EPSG:7844)
    Geo bounding box {"type":"Polygon","coordinates":[[[137.5,-30],[138,-30],[138,-29.5],[137.5,-29.5],[137.5,-30]]]}
    Purpose 
    
                    
                    
    
                    
                      		
                
    
              
                
                
    
                  
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