Physical processes in Subglacial Lake Whillans, West Antarctica: Inferences from sediment cores
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文摘

A first look inside a dynamic hydrologic network beneath the Whillans Ice Plain.

No evidence of energetic flow within the subglacial drainage network.

Sediment on the lake floor consists of till deposited when the ice stream grounds.

Fabrics within the till suggest shallow deformation of the Whillans Ice Plain.

Low sediment fluxes to the grounding zone are unlikely to stabilize the ice stream.

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