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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ftciteseerx:oai:CiteSeerX.psu:10.1.1.666.2398 2023-05-15T16:35:14+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf 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 en eng 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 Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://lgm.ggr.ulaval.ca/wp-content/uploads/2011/12/Lajeunesse_2008.pdf Deglaciation Glaciomarine environment Glacial landforms Ice-contact submarine fans Laure text ftciteseerx 2016-01-08T17:06:31Z 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 Text Hudson Bay Keewatin Unknown Hudson Hudson Bay Laure ENVELOPE(-63.350,-63.350,-64.767,-64.767) Vio ENVELOPE(-61.283,-61.283,-64.083,-64.083) |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
topic |
Deglaciation Glaciomarine environment Glacial landforms Ice-contact submarine fans Laure |
spellingShingle |
Deglaciation Glaciomarine environment Glacial landforms Ice-contact submarine fans Laure |
topic_facet |
Deglaciation Glaciomarine environment Glacial landforms Ice-contact submarine fans Laure |
description |
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 |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
url |
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 |
long_lat |
ENVELOPE(-63.350,-63.350,-64.767,-64.767) ENVELOPE(-61.283,-61.283,-64.083,-64.083) |
geographic |
Hudson Hudson Bay Laure Vio |
geographic_facet |
Hudson Hudson Bay Laure Vio |
genre |
Hudson Bay Keewatin |
genre_facet |
Hudson Bay Keewatin |
op_source |
http://lgm.ggr.ulaval.ca/wp-content/uploads/2011/12/Lajeunesse_2008.pdf |
op_relation |
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 |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766025416115486720 |