Evaluating quaternary glacial till sheet volume and duration of grounding events using sediment flux calculations in the Eastern basin paleotroughs, Ross Sea, Anarctica
A sequence of three seismically-resolvable, back-stepping grounding zone wedges (GZWs) within the Glomar-Challenger Basin paleo-ice-stream trough is conventionally interpreted to have been deposited by the West Antarctic Ice Sheet (WAIS) since the end of the Last Glacial Maximum (LGM). For this to b...
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LSU Digital Commons
2013
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| Online Access: | https://digitalcommons.lsu.edu/gradschool_theses/65 https://doi.org/10.31390/gradschool_theses.65 https://digitalcommons.lsu.edu/context/gradschool_theses/article/1064/viewcontent/uc.pdf |