Authors / CoAuthors
Sullivan, C.J. | Dallwitz, W.B.
Abstract
The existence of wolfram in the deposit has been known since about 1915, and mining was carried out intermittently from that time until about 1938. It was not until June, 1951, when the deposit was visited by us, that the existence of scheelite in important quantity in the known ore was established. During this visit, also, a study of the structure of the deposit convinced us that, although only a little ore was exposed, considerable quantities of non-outcropping ore might be found. As magnetite is one of the gangue-minerals, a request was made for a magnetic survey. This survey was carried out by the Geophysical Section. Subsequent diamond drilling by Tungsten Consolidated Limited has shown that substantial bodies of scheelite and wolfram ore exist in the area under the structural conditions originally postulated; these conditions are outlined below. The geology of the deposits and the results of combined geological, geophysical, and diamond drilling investigations are discussed.
Product Type
document
eCat Id
9334
Contact for the resource
Custodian
Owner
Custodian
Cnr Jerrabomberra Ave and Hindmarsh Dr GPO Box 378
Canberra
ACT
2601
Australia
Keywords
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- GA PublicationRecord
- ( Theme )
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- geology
- ( Theme )
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- mineral deposits
- ( Theme )
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- ore
- ( Theme )
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- resource assessment
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- AU-NSW
- Australian and New Zealand Standard Research Classification (ANZSRC)
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- Geology
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- Published_External
Publication Date
1952-01-01T00:00:00
Creation Date
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Status
Purpose
Maintenance Information
unknown
Topic Category
geoscientificInformation
Series Information
Record 1952/054
Lineage
Legacy product, lineage not available
Parent Information
Extents
[-34.6, -34.4, 148.8, 149.0]
Reference System
Spatial Resolution
Service Information
Associations
Source Information
Legacy product, source data not available.