Rock geochemical exploration at Mount Morgan, Queensland, Australia |
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| Authors: | M Fedikow GJS Govett |
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| Abstract: | The Mount Morgan Au-Cu pyritic sulphide deposit occurs in a north-northwest trending belt of Middle Paleozoic volcanic rocks located in south-central Queensland. This volcanic belt forms part of the Yarrol Basin in the Northern New England Fold Belt of the East Australian Tasman Geosyncline. The host rocks for the deposit are a normal sequence of rhyolitic and dacitic tuff that have a north-northwest regional strike and easterly dips of 20° to 30°. The tuff contains thin units of cert, jasperoid and carbonate rocks. |
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