Neoarchean evolution of the western-central Wabigoon boundary zone, Brightsand Forest Area, Ontario.
The boundary between the western and central domains of the Wabigoon subprovince has been considered to represent a ca. 2.7 Ga suture between juvenile Neoarchean volcanic rocks in the west and granitoid rocks with Mesoarchean ancestry in the central Wabigoon. The nature and timing of interaction bet...
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University of Ottawa (Canada)
2009
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| Online Access: | http://hdl.handle.net/10393/6451 http://dx.doi.org/10.20381/ruor-11282 |