Evidence for multiple quaternary ice advances and fan development from the amundsen gulf cross-shelf trough and slope, canadian beaufort sea margin

Marine and Petroleum Geology

Volumn 52, Issue , 2014, Pages 125-143

  Batchelor, C L ^a   Dowdeswell, J A ^a   Pietras, J T ^b  

^a UNIVERSITY OF CAMBRIDGE   (United Kingdom)

^b BINGHAMTON UNIVERSITY   (United States)

Author keywords

Amundsen Gulf; Grounding zone wedge; Ice stream; Laurentide Ice Sheet; Seismic reflection; Trough mouth fan

Indexed keywords

GLACIERS; LANDFORMS; SEDIMENTS; SEISMIC WAVES; SEISMOLOGY; STRATIGRAPHY; SUBMARINE GEOLOGY;

AMUNDSEN GULF; GROUNDING-ZONE WEDGES; ICE STREAMS; LAURENTIDE ICE SHEETS; SEISMIC REFLECTIONS;

ICE;

BEDROCK; GLACIOMARINE DEPOSIT; ICE FLOW; ICE STREAM; LAST DEGLACIATION; LAURENTIDE ICE SHEET; QUATERNARY; SEISMIC DATA; SEISMIC STRATIGRAPHY; TWO-DIMENSIONAL MODELING;

AMUNDSEN GULF; ARCTIC OCEAN; BEAUFORT SEA;

EID: 84895861946     PISSN: 02648172     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.marpetgeo.2013.11.005     Document Type: Article

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