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RB 91/00095 Recrystallised dolomites from the Tarcoola region.
Published: 01 Oct 1991 Created: 07 Nov 2024 Revised: 07 Nov 2024
Author: Farrand, M.G.

Progressive alteration through recrystallisation without significant metasomatism or dynamic metamorphism has taken place in 8 specimens of what are assumed to be original sedimentary dolomites. The present paragenesis includes talc and chlorites...

Progressive alteration through recrystallisation without significant metasomatism or dynamic metamorphism has taken place in 8 specimens of what are assumed to be original sedimentary dolomites. The present paragenesis includes talc and chlorites of both penninite and antigorite affinities. A zeolite forms inclusions in veins of coarsely recrystallised dolomite. Minor sphene and pseudomorphs after pyrite are present.

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About this record

Record No rb9100095
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 carbonaceous material
Notes 
Geographic Locality: Tarcoola
Doc No: RB 91/00095
Geographic Locality: Tarcoola
Doc No: RB 91/00095
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/rb9100095
Citation Farrand, M.G. 1991. RB 91/00095 Recrystallised dolomites from the Tarcoola region. Departmental Publication - Geological Survey Geoscience Publication. Government of South Australia.
https://pid.sarig.sa.gov.au/document/rb9100095

Technical information

Status
Maintenance and Update Frequency
Geographic Reference GDA2020 (EPSG:7844)
Geo bounding box {"type":"Polygon","coordinates":[[[134.5,-31],[135,-31],[135,-30.5],[134.5,-30.5],[134.5,-31]]]}
Purpose 

                    
                    

                    
                  		
                

              
                
                

                  
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