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Progress and final reports on biostratigraphic mapping in the Gambier - Northumberland district from March 1960 to 22/11/1960.
Published: 01 Jan 1960 Created: 13 Nov 2024 Revised: 13 Nov 2024
Author: Abele, C.

Recognition of foraminiferal zones confirms the closure of the structural high near Mount Salt Homestead in a northwesterly direction, and suggest that its NE boundary is at least partly formed by en echelon faults extending in a roughly NW...

Recognition of foraminiferal zones confirms the closure of the structural high near Mount Salt Homestead in a northwesterly direction, and suggest that its NE boundary is at least partly formed by en echelon faults extending in a roughly NW direction.

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About this record

Record No mesac36050
Topic Geoscientific Information
Type of Resource Document
Category Type
Document Type Energy Company Report - Annual licence or technical report
Contributor
Sponsor
Tenement OEL 22
Tenement Holder General Exploration Co. Australia Pty Ltd
Operator General Exploration Co. Australia Pty Ltd
Geological Province Otway Basin
Mine Name
Stratigraphy Gambier Limestone
Commodity
    Notes 
    Doc No: Env 00019 R2 p: 10-21
    Doc No: Env 00019 R2 p: 10-21
    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/mesac36050
    Citation Abele, C. 1960. Progress and final reports on biostratigraphic mapping in the Gambier - Northumberland district from March 1960 to 22/11/1960. Energy Company Report - Annual licence or technical report
    https://pid.sarig.sa.gov.au/document/mesac36050

    Technical information

    Status
    Maintenance and Update Frequency
    Geographic Reference GDA2020 (EPSG:7844)
    Geo bounding box {"type":"Polygon","coordinates":[[[140.5,-38.5],[141,-38.5],[141,-37.5],[140.5,-37.5],[140.5,-38.5]]]}
    Purpose 
    
                    
                    
    
                    
                      		
                
    
              
                
                
    
                  
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