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RB 55/00129 Imbitcha clay deposit.
Published: 01 Jan 1964 Created: 05 Nov 2024 Revised: 05 Nov 2024
Author: Heath, G.R.

Imbitcha clay deposit occurs in marine Cretaceous shales which have been incorporated in the basal mottled zone of a laterite profile. Reserves may total millions of tons, but problems of extraction and the alunite content of the clay probably...

Imbitcha clay deposit occurs in marine Cretaceous shales which have been incorporated in the basal mottled zone of a laterite profile. Reserves may total millions of tons, but problems of extraction and the alunite content of the clay probably make it uneconomic to exploit at present.

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About this record

Record No rb5500129
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 Arckaringa Basin
Mine Name
Stratigraphy
Commodity
Notes 
Notes: Published by SADM in: Mining Review, Adelaide. No. 117 (1964); p: 38-42 474/00556
Geographic Locality: Imbitcha;Arckaringa
Doc No: RB 55/00129
Notes: Published by SADM in: Mining Review, Adelaide. No. 117 (1964); p: 38-42 474/00556
Geographic Locality: Imbitcha;Arckaringa
Doc No: RB 55/00129
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/rb5500129
Citation Heath, G.R. 1964. RB 55/00129 Imbitcha clay deposit. Departmental Publication - Geological Survey Geoscience Publication. Government of South Australia.
https://pid.sarig.sa.gov.au/document/rb5500129

Technical information

Status
Maintenance and Update Frequency
Geographic Reference GDA2020 (EPSG:7844)
Geo bounding box {"type":"Polygon","coordinates":[[[133.5,-28],[135,-28],[135,-27],[133.5,-27],[133.5,-28]]]}
Purpose 

                    
                    

                    
                  		
                

              
                
                

                  
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