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RB 78/00090 Olivine basalt dyke near Terowie. Hd Terowie Co. Kimberley.
Published: 31 Jul 1978 Created: 06 Nov 2024 Revised: 06 Nov 2024
Author: Carr, S.G.;Olliver, J.G.

This discordant dyke related to kimberlite and carbonatite intrusions has been emplaced at a low temperature into Umberatana Group shales and siltstones. Its composition is unsuitable for use in manufacturing glass and ceramics due to both low...

This discordant dyke related to kimberlite and carbonatite intrusions has been emplaced at a low temperature into Umberatana Group shales and siltstones. Its composition is unsuitable for use in manufacturing glass and ceramics due to both low nepheline and high iron contents.

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About this record

Record No rb7800090
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 Adelaide Geosyncline
Mine Name
Stratigraphy Tapley Hill Formation
Commodity
Notes 
Geographic Locality: Terowie;Hallett;Franklin;Waupunyah Creek
Doc No: RB 78/00090
Geographic Locality: Terowie;Hallett;Franklin;Waupunyah Creek
Doc No: RB 78/00090
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/rb7800090
Citation Carr, S.G.;Olliver, J.G. 1978. RB 78/00090 Olivine basalt dyke near Terowie. Hd Terowie Co. Kimberley. Departmental Publication - Geological Survey Geoscience Publication. Government of South Australia.
https://pid.sarig.sa.gov.au/document/rb7800090

Technical information

Status
Maintenance and Update Frequency
Geographic Reference GDA2020 (EPSG:7844)
Geo bounding box {"type":"Polygon","coordinates":[[[139,-33.5],[139.5,-33.5],[139.5,-33],[139,-33],[139,-33.5]]]}
Purpose 

                    
                    

                    
                  		
                

              
                
                

                  
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