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Subglacial sediment transport upstream of a basal channel in the ice shelf of Support Force Glacier (West Antarctica), identified by reflection seismics (2020)

First Author: Hofstede C

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