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RB 65/00025 Tertiary foraminiferal zones in South Australia.
Published: 01 Jan 1968 Created: 05 Nov 2024 Revised: 05 Nov 2024
Author: Ludbrook, N.H.;Lindsay, J.M.

A continuous succession of fifteen planktonic foraminiferal zones is proposed for Middle Eocene to Miocene sediments in South Australia. With some slight modification the zonal scheme is closely identified with a similar succession In New Zealand....

A continuous succession of fifteen planktonic foraminiferal zones is proposed for Middle Eocene to Miocene sediments in South Australia. With some slight modification the zonal scheme is closely identified with a similar succession In New Zealand. Two alternative zones are useful for the Oligocene in areas of restricted sedimentation.

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Record No rb6500025
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
Stratigraphy
Commodity
    Notes 
    Notes: 66/01648
Geographic Locality: South Australia;Africa
Doc No: RB 65/00025
    Notes: 66/01648
Geographic Locality: South Australia;Africa
Doc No: RB 65/00025
    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/rb6500025
    Citation Ludbrook, N.H.;Lindsay, J.M. 1968. RB 65/00025 Tertiary foraminiferal zones in South Australia. Departmental Publication - Geological Survey Geoscience Publication. Government of South Australia.
    https://pid.sarig.sa.gov.au/document/rb6500025

    Technical information

    Status
    Maintenance and Update Frequency
    Geographic Reference GDA2020 (EPSG:7844)
    Geo bounding box {"type":"Polygon","coordinates":[[[129,-39],[141,-39],[141,-26],[129,-26],[129,-39]]]}
    Purpose 
    
                    
                    
    
                    
                      		
                
    
              
                
                
    
                  
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