Mineralogical and chemical evolution of the Ernest Henry Fe oxide–Cu–Au ore system, Cloncurry district, northwest Queensland, Australia-Reference-Cited by-同舟云学术

Mineralogical and chemical evolution of the Ernest Henry Fe oxide–Cu–Au ore system, Cloncurry district, northwest Queensland, Australia

Published:2006-02-01 Issue:8 Volume:40 Page:769-801
ISSN:0026-4598
Container-title:Mineralium Deposita
language:en
Short-container-title:Miner Deposita

Author:

Mark Geordie,Oliver Nicholas H. S.,Williams Patrick J.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Link

http://link.springer.com/content/pdf/10.1007/s00126-005-0009-7.pdf

Reference103 articles.

1. Adshead ND (1995) Geology, alteration and geochemistry of the Osborne Cu–Au deposit, Cloncurry district, NW Queensland. PhD thesis, unpublished. James Cook University

2. Adshead ND (1996) The role of hypersaline hydrothermal fluids in the formation of the Osborne Cu–Au deposit, Cloncurry district, NW Queensland. EGRU Contrib 55:1–4

3. Aitkin BP, Injque-Espinoza JL, Harvey PK (1985) Cu–Fe-amphibole mineralization in the Arequipa segment. In: Pitcher WS et al (eds) Magmatism at a plate edge: the Peruvian Andes. Blackie, Glasgow, pp 261–270

4. Audétat A, Günthur D, Heinrich CA (2000) Magmatic-hydrothermal evolution in a fractionating granite: a microchemical study of the Sn-W-F-mineralized Mole Granite (Australia). Econ Geol 95:1563–1581

5. Badham JPN (1978) Magnetite-apatite-amphibole-uranium and silver-arsenide mineralizations in Lower Proterozoic igneous rocks, East Arm, Great Slave Lake, Canada. Econ Geol 73:1474–1491

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