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Nature and longevity of hydrothermal fluid flow and mineralisation in granites of the Bushveld Complex, South Africa

Robb, L; Freeman, L; Armstrong, Richard


The Lebowa Granite Suite of the Bushveld Complex is a large, 2054 Ma old, A-type Batholith, characterised by numerous relatively small magmato-hydrothermal, polymetallic ore Deposits. The mineralisation is represented by a three-stage paragenetic sequence: early magmatic Sn-W-Mo-F ores (600 °C > T > 400 °C), followed by a Cu-Pb-Zn-As-Ag-Au paragenesis (400 °C > T > 200 °C) and then late-stage Fe-F-U mineralisation (< 200 °C). The first stage of Mineralisation (typified by the endogranitic...[Show more]

CollectionsANU Research Publications
Date published: 2000
Type: Journal article
Source: Transactions of the Royal Society of Edinburgh: Earth Sciences
DOI: 10.1130/0-8137-2350-7.269


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