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The fluorine link between a supergiant ore deposit and a silicic large igneous province: Forum Reply

journal contribution
posted on 2023-05-26, 11:05 authored by Jocelyn McPhieJocelyn McPhie, Vadim Kamenetsky, Allen, S, Ehrig, K, Agangi, A, Bath, A
Manning (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

Geology

Volume

40

Article number

8

Number

8

Pagination

e276

ISSN

0091-7613

Publication status

  • Published

Rights statement

Copyright 2012 Geological Society of America

Repository Status

  • Restricted

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