Sedimentology and chronology of the advance and retreat of the last British-Irish Ice Sheet on the continental shelf west of Ireland
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文摘

Our findings characterise BIIS behaviour during retreat.

New radiocarbon ages constrain retreat rates.

Multiple lines of evidence identify a mid-shelf stillstand.

Geomorphology identifies retreat phase thinning and reconfiguration.

Ice shelf buttressing slowed initial grounding zone retreat.

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