High-temperature metasomatism driven by ascent of voluminous, saline fluid columns in the upper crust plays a major role in the genesis of iron oxide-alkali...
Canadian Institute of Mining. Metallurgy and Petroleum (CIM)
The eight papers presented in this issue of Exploration & Mining Geology arose primarily from presentations made in a Special Session at the GeoCanada 2010...
The Chisel Lake deposit, in the Flin Flon - Snow Lake Mineral Belt in northern Manitoba, is characterized by an ore mineral assemblage dominated by pyrite and...
The basement-hosted Bong uranium deposit in the Kiggavik region is associated with a broad hydrothermal alteration halo characterized by an inner illite-rich...
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 Paleoproterozoic East Arm Basin of Canada hosts polymetallic vein, iron oxide-apatite (IOA), and potential iron oxide-copper-gold (IOCG) mineral...
The essential ingredients required to form any 'basin-related' uranium deposit are a source of oxidizing, U(VI)-bearing fluids and a mechanism to reduce mobile...
The basement rocks along the P2 fault are extensively altered, particularly where they host the McArthur River Zone 2 uranium ore body. Two generations of...
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