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RB 80/00019 Microstructural development of mylonites near Cowell, eastern Eyre Peninsula, South Australia.
Published: 01 Jan 1980 Created: 06 Nov 2024 Revised: 06 Nov 2024
Author: Parker, A.J.

Reports on part of major structural study. The mylonite zone has developed by progressive deformation and recrystal- lization of high grade gneisses during regional fold event. The micro- structural development corresponds with sequence of...

Reports on part of major structural study. The mylonite zone has developed by progressive deformation and recrystal- lization of high grade gneisses during regional fold event. The micro- structural development corresponds with sequence of recrystallization from quartz to mylonite zone to mica within mylonitized gneisses, then feldspar within slaty mylonite within the zone.

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About this record

Record No rb8000019
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 industrial material
Notes 
Geographic Locality: Cowell;Cleve Uplands
Doc No: RB 80/00019
Geographic Locality: Cowell;Cleve Uplands
Doc No: RB 80/00019
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/rb8000019
Citation Parker, A.J. 1980. RB 80/00019 Microstructural development of mylonites near Cowell, eastern Eyre Peninsula, South Australia. Departmental Publication - Geological Survey Geoscience Publication. Government of South Australia.
https://pid.sarig.sa.gov.au/document/rb8000019

Technical information

Status
Maintenance and Update Frequency
Geographic Reference GDA2020 (EPSG:7844)
Geo bounding box {"type":"Polygon","coordinates":[[[136.5,-34],[137,-34],[137,-33.5],[136.5,-33.5],[136.5,-34]]]}
Purpose 

                    
                    

                    
                  		
                

              
                
                

                  
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