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The fluorine link between a supergiant ore deposit and a silicic large igneous province: Forum Reply
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posted on 2023-05-26, 11:05 authored by Jocelyn McPhieJocelyn McPhie, Vadim Kamenetsky, Allen, S, Ehrig, K, Agangi, A, Bath, AManning (2012) has challenged our suggestion that dissolution by hydrofl uoric acid (HF) contributed to the formation of the Olympic Dam breccia complex (McPhie et al., 2011b). Manning has summarized the outcome of considerable experimental and other research on HF-granite interactions under magmatic and near-magmatic temperature and pressure conditions. Under these conditions, a reaction takes place, rather than dissolution, and produces a crystalline quartz-topaz assemblage. However, these conditions are not relevant to our proposal that HF played a role in the formation of the Olympic Dam breccia complex.
History
Publication title
GeologyVolume
40Article number
8Number
8Pagination
e276ISSN
0091-7613Publication status
- Published
Rights statement
Copyright 2012 Geological Society of AmericaRepository Status
- Restricted
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