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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| Format: | Text |
| Language: | English |
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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 |
| Summary: | 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 available regarding the possible continuation of the NastapokaDrift belt was constructed during the relative sea level of the QLIS in eastern Hudson Bay during deglaciation. This paper builds upon previous regional investigations |
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