th aj hie rm 2 14 ne c vio demonstrated that during the relative sea level highstand that shortly followed the drainage of the lake, the western margin of the Québec– (LIS) into the Keewatin Ice Sector (KIS) to the west and the eastern Hudson Bay (Lajeunesse and Allard, 2002, 2003a,b). No data is av...
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.666.2398 http://lgm.ggr.ulaval.ca/wp-content/uploads/2011/12/Lajeunesse_2008.pdf |