Subglacial sediment transport upstream of a basal channel in the ice shelf of Support Force Glacier (West Antarctica), identified by reflection seismics (2020)
Attributed to:
Ice shelves in a warming world: Filchner Ice Shelf system, Antarctica
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.5194/tc-2020-54
Publication URI: http://dx.doi.org/10.5194/tc-2020-54
Type: Preprint