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

Uranium and polymetallic U mineralization hosted within brecciated albitites occurs one kilometer south of the magnetite-rich Au–Co–Bi–Cu NICO deposit in the southern Great Bear magmatic zone (GBMZ), Canada. Concentrations up to 1 wt% U are distributed throughout a 3 by 0.5 km albitization corridor...

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Bibliographic Details
Published in:Mineralium Deposita
Main Authors: Montreuil, Jean-François, Corriveau, Louise, Potter, Eric G.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2015
Subjects:
Online Access:https://espace.inrs.ca/id/eprint/4325/
https://doi.org/10.1007/s00126-014-0530-7