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RB 83/00082 Proterozoic intrusives, Streaky Bay area.
Published: 01 Oct 1983 Created: 06 Nov 2024 Revised: 06 Nov 2024
Author: Watkins, N.L.;Flint, R.B.

The intrusives are dominated by granite, N - S oriented diorite dykes up to 50 metres wide, and late stage aplitic and pegmatitic veins with variable orientation. A Middle Proterozoic age is indicated for some of the granitoids, which were...

The intrusives are dominated by granite, N - S oriented diorite dykes up to 50 metres wide, and late stage aplitic and pegmatitic veins with variable orientation. A Middle Proterozoic age is indicated for some of the granitoids, which were probably intruded during the final stages of the Kimban Orogeny.

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About this record

Record No rb8300082
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 Gawler Craton
Mine Name
Stratigraphy
Commodity
    Notes 
    Geographic Locality: Streaky Bay;Ceduna;Point Brown;Point Westall
Doc No: RB 83/00082
    Geographic Locality: Streaky Bay;Ceduna;Point Brown;Point Westall
Doc No: RB 83/00082
    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/rb8300082
    Citation Watkins, N.L.;Flint, R.B. 1983. RB 83/00082 Proterozoic intrusives, Streaky Bay area. Departmental Publication - Geological Survey Geoscience Publication. Government of South Australia.
    https://pid.sarig.sa.gov.au/document/rb8300082

    Technical information

    Status
    Maintenance and Update Frequency
    Geographic Reference GDA2020 (EPSG:7844)
    Geo bounding box {"type":"Polygon","coordinates":[[[133.5,-33],[134.5,-33],[134.5,-32],[133.5,-32],[133.5,-33]]]}
    Purpose 
    
                    
                    
    
                    
                      		
                
    
              
                
                
    
                  
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