The sediment drifts of the Antarctic Peninsula Pacific margin (Fig. 1) are a systematic component of a distinctive, fully glacial pattern of sediment transport and deposition. Terrigenous sediment supply is provided during glacial maxima by grounded ice sheets transporting unsorted tills to the continental shelf edge.
Sediment Drifts on the Continental Rise of the Antarctic Peninsula
Rebesco, Michele;Camerlenghi, Angelo
1997-01-01
Abstract
The sediment drifts of the Antarctic Peninsula Pacific margin (Fig. 1) are a systematic component of a distinctive, fully glacial pattern of sediment transport and deposition. Terrigenous sediment supply is provided during glacial maxima by grounded ice sheets transporting unsorted tills to the continental shelf edge.File in questo prodotto:
Non ci sono file associati a questo prodotto.
I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.