A fluid inclusion study of the Suicide Ridge Breccia Pipe, Cloncurry district, Australia: Implication for Breccia Genesis and IOCG mineralization

Author:

Bertelli Martina,Baker Timothy

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference88 articles.

1. Adshead, N.D., 1996. The role of hypersaline hydrothermal fluids in the formation of the Osborne Cu-Au deposit, Cloncurry District, NW Queensland. In: Baker, T., Rotherham, J.F., Richmond, J.M., Mark, G., Williams, P.J. (Eds.), MIC 96’; New Developments in Metallogenic Research; The McArthur-Mount Isa-Cloncurry Minerals Province. James Cook University, Townsville. EGRU Contribution 55, pp. 1–4.

2. Adshead, N.D., Voulgaris, P., Muscio, V.N., 1998. Osborne copper-gold deposit. In: Berkman, D.A., Mackenzie, D.H. (Eds.), Geology of Australian and Papua New Guinean Mineral Deposits. Australasian Institute of Mining Monograph Series 22, pp. 793–799.

3. Alteration, mineralization, and fluid evolution at the Eloise Cu-Au deposit, Cloncurry District, Northwest Queensland, Australia;Baker;Economic Geology,1998

4. Emplacement depth and carbon dioxide-rich fluid inclusions in intrusion-related deposits;Baker;Economic Geology,2002

5. The Eloise Cu-Au deposit, East Mt Isa Block: structural environment and structural controls on ore;Baker;Australian Journal of Earth Sciences,1998

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