Authors / CoAuthors
Bagas, L.
Abstract
Presented at the Evolution and metallogenesis of the North Australian Craton Conference, 20-22 June 2006, Alice Springs. The ca 1864 Ma Stubbins Formation is a sequence of turbiditic and mafic volcanic rocks that were informally called the Bald Hill sequence. The formation hosts the Kookaburra and Sandpiper deposits and a number of smaller prospects in the Bald Hill area of Western Australia. The ca 1835 Ma turbiditic Killi Killi Formation hosts the Coyote deposit and several nearby prospects. <p>Related product:<a href="https://www.ga.gov.au/products/servlet/controller?event=GEOCAT_DETAILS&catno=64764">Evolution and metallogenesis of the North Australian Craton Conference Abstracts</p>
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nonGeographicDataset
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70498
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- PowerPoint
- ( Theme )
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- gold
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- AU-WA
- Australian and New Zealand Standard Research Classification (ANZSRC)
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- Earth Sciences
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- Published_Internal
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2006-01-01T00:00:00
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