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EPMA monazite constraints on the timing of deformation and metamorphism in the southern Kalinjala Shear Zone, Gawler Craton.
Created: 29 Oct 2024 Revised: 07 Dec 2024
Author: Dutch, R.A.;Hand, M.P.

In this article we present new EPMA monazite geochronological data from the deformed and metamorphosed Sleaford Complex units at Fishery Bay in the southern Gawler Craton. The results show that these fabrics formed during the development of the...

In this article we present new EPMA monazite geochronological data from the deformed and metamorphosed Sleaford Complex units at Fishery Bay in the southern Gawler Craton. The results show that these fabrics formed during the development of the Kalinjala Shear Zone during the 1725?1690 Ma Kimban Orogeny.

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About this record

Record No mesac22008
Topic Geoscientific Information
Type of Resource Document
Category Type
Document Type Departmental Publication - MESA Journal
Contributor
Sponsor
Tenement
Tenement Holder
Operator
Geological Province Gawler Craton
Mine Name
Stratigraphy Sleaford Complex
Commodity
    Notes 
    Geographic Locality: Kalinjala Shear Zone
Doc No: MESAJ 053 p: 041-046
    Geographic Locality: Kalinjala Shear Zone
Doc No: MESAJ 053 p: 041-046
    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/mesac22008
    Citation Dutch, R.A.;Hand, M.P. EPMA monazite constraints on the timing of deformation and metamorphism in the southern Kalinjala Shear Zone, Gawler Craton. Departmental Publication - Mesa Journal. Government of South Australia.
    https://pid.sarig.sa.gov.au/document/mesac22008

    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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