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...

Full description

Bibliographic Details
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Deglaciation
Glaciomarine environment
Glacial landforms
Ice-contact submarine fans
Laure
Hudson
Hudson Bay
Vio
Keewatin
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
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.666.2398
record_format openpolar
spelling 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

Similar Items