Trace element composition of iron oxides from IOCG and IOA deposits: relationship to hydrothermal alteration and deposit subtypes-Reference-Cited by-同舟云学术

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Trace element composition of iron oxides from IOCG and IOA deposits: relationship to hydrothermal alteration and deposit subtypes

Published:2018-07-17 Issue:4 Volume:54 Page:525-552
ISSN:0026-4598
Container-title:Mineralium Deposita
language:en
Short-container-title:Miner Deposita

Author:

Huang Xiao-Wen,Boutroy Émilie,Makvandi Sheida,Beaudoin Georges,Corriveau Louise,De Toni Anthony Franco

Funder

China Scholarship Council

Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada

Agnico Eagle Mines Limited

Ministry of Natural Resources

Natural Resources Canada

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Link

http://link.springer.com/content/pdf/10.1007/s00126-018-0825-1.pdf

Reference143 articles.

1. Acosta-Góngora P, Gleeson S, Samson I, Ootes L, Corriveau L (2014) Trace element geochemistry of magnetite and its relationship to Cu-Bi-Co-Au-Ag-UW mineralization in the Great Bear magmatic zone, NWT, Canada. Econ Geol 109:1901–1928

2. Aitchison J (1986) The statistical analysis of compositional data. Chapman and Hall Ltd., London, UK, pp 1–416

3. Angerer T, Hagemann SG, Danyushevsky LV (2012) Geochemical evolution of the banded iron formation-hosted high-grade iron ore system in the Koolyanobbing Greenstone Belt, Western Australia. Econ Geol 107:599–644

4. Apukhtina OB, Kamenetsky VS, Ehrig K, Kamenetsky MB, Maas R, Thompson J, McPhie J, Ciobanu CL, Cook NJ (2017) Early, deep magnetite–fluorapatite mineralization at the Olympic dam Cu-U-Au-Ag deposit, South Australia. Econ Geol 112:1531–1542

5. Barnes SJ, Roeder PL (2001) The range of spinel compositions in terrestrial mafic and ultramafic rocks. J Petrol 42:2279–2302

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