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RB 80/00119 Drew Hill pegmatite, Olary Province.
Published: 01 Sep 1980 Created: 06 Nov 2024 Revised: 06 Nov 2024
Author: Conor, C.H.H.;Harris, R.J.

A pegmatite deposit located 1 km south of Cathedral Rock and 1.5 km north-west of Drew Hill was investigated by surveying, mapping and rock chip sampling. This Drew Hill pegmatite, which is 200 metres long and 45 metres wide, is enclosed by...

A pegmatite deposit located 1 km south of Cathedral Rock and 1.5 km north-west of Drew Hill was investigated by surveying, mapping and rock chip sampling. This Drew Hill pegmatite, which is 200 metres long and 45 metres wide, is enclosed by quartz-feldspar-mica schist of the Willyama Complex. The pegmatite is an unzoned quartz-perthite-albite-muscovite body, with limited mineable feldspar reserves and a variable mineral composition.

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About this record

Record No rb8000119
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 Willyama Inliers
Mine Name Drew Hill pegmatite deposit
Stratigraphy
Commodity industrial material
Notes 
Geographic Locality: Bimbowrie Station
Doc No: RB 80/00119
Geographic Locality: Bimbowrie Station
Doc No: RB 80/00119
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/rb8000119
Citation Conor, C.H.H.;Harris, R.J. 1980. RB 80/00119 Drew Hill pegmatite, Olary Province. Departmental Publication - Geological Survey Geoscience Publication. Government of South Australia.
https://pid.sarig.sa.gov.au/document/rb8000119

Technical information

Status
Maintenance and Update Frequency
Geographic Reference GDA2020 (EPSG:7844)
Geo bounding box {"type":"Polygon","coordinates":[[[140,-32.5],[140.5,-32.5],[140.5,-32],[140,-32],[140,-32.5]]]}
Purpose 

                    
                    

                    
                  		
                

              
                
                

                  
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