Formation of albitite-hosted uranium within IOCG systems: the Southern Breccia, Great Bear magmatic zone, Northwest Territories, Canada

Author:

Montreuil Jean-François,Corriveau Louise,Potter Eric G.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Reference89 articles.

1. Acosta GP, Gleeson SA, Taylor B, Samson I, Ootes L, Corriveau L (2013) Sulfur isotope geochemistry and 187Re–187Os temporal constraints on the formation of polymetallic iron-oxide-alkali-altered deposits in the Great Bear magmatic zone, NWT, Canada. SGA2013–The 12th Biennial SGA Meeting of The Society for Geology Applied to Ore Deposits, Upsala, Sweden, Transaction volume

2. Acosta GP, Gleeson SA, Samson I, Ootes L, Corriveau L (2014) Trace element geochemistry of magnetite and its relationship to Cu-Bi-Co-Au-Ag-U-W mineralization in the Great Bear magmatic zone, NWT, Canada. Econ Geol, in press.

3. Adams JAS, Fryer GE (1964) Portable γ-ray spectrometer for field determination of thorium, uranium and potassium. In: Lowder WM, Adams JAS (eds) The natural radiation environment. University of Chicago Press, Chicago, pp 577–596

4. Aitchison J (1986) The statistical analysis of compositional data. Chapman & Hall, London, 416p

5. Aja SU, Wood SA, Williams-Jones AE (1995) The aqueous geochemistry of Zr and the solubility of some Zr-bearing minerals. Appl Geochem 10:603–620

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