Authors / CoAuthors
Davis, B. | Blewett, R.S. | Squire, R. | Champion, D.C. | Henson, P.A.
Abstract
Archaean domes are associated with many of the larger gold deposits of the Eastern Goldfields Superterrane (e.g., Sunrise Dam, Wallaby, St Ives camp, Kalgoorlie, Lawlers etc), and the Scotia-Kanowna Dome is eroded to sufficiently deep levels to provide insights into the role domes play in controlling gold deposition. At the centre of the Scotia-Kanowna Dome is a granite-cored batholith, which is surrounded by outward-dipping greenstone belts and associated shear zones. A number of small- to medium-sized gold deposits occur on the limbs and the centre of the dome, and the world-class Kanowna Belle gold mine occurs on the nose of the dome. At least three separate gold mineralising events are defined, each of regional significance that can be correlated with other well known gold deposits of the Eastern Goldfields Superterrane. The architecture of granite-cored domes has played a critical role in focussing magma as well as mineralising fluids into regions of maximum dilation. They do this by nature of their inherent competence, by influencing the position and geometry of shear zones (fluid pathways) and hence distribution of stratigraphy (depositional sites) across the region. The Scotia-Kanowna Dome is a good example to study this control, and inferences can be made for similar controls by concealed domes, such as beneath Kalgoorlie.
Product Type
nonGeographicDataset
eCat Id
68828
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Custodian
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Cnr Jerrabomberra Ave and Hindmarsh Dr GPO Box 378
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Keywords
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- External Publication
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- 3D model
- ( Theme )
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- mineral deposits
- ( Theme )
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- structural geology
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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
Publication Date
2009-04-20T00:00:00
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geoscientificInformation
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[-30.0, -29.0, 122.0, 124.0]
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Spatial Resolution
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