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(Fig. 3f) Shear strength of sediment core JR104-GC371
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(Supp. Fig.) Shear strength of sediment core JR104-GC370
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(Supp. Fig.) Shear strength of sediment core JR104-GC368
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(Fig. 3a) Shear strength of sediment core JR104-GC366
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(Supp. Fig.) Shear strength of sediment core JR104-GC365
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(Supp. Fig.) Shear strength of sediment core JR104-GC362
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(Fig. 3b) Shear strength of sediment core JR104-GC360
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(Fig. 3c) Shear strength of sediment core JR104-GC359
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(Supp. Fig.) Shear strength of sediment core JR104-GC358
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(Fig. 3d) Shear strength of sediment core JR104-GC357
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(Supp. Fig.) Shear strength of sediment core JR104-GC352
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(Fig. 2) Clay mineral composition of seabed surface sediments
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(Table 1) Distribution of tephra layers in sediment cores from the Bellingsha...
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Magnetic susceptibility of sediment core GC378 from the West Antarctic contin...
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Sedimentology of the southern Bellingshausen Sea
A major trough ('Belgica Trough') eroded by a palaeo-ice stream crosses the continental shelf of the southern Bellingshausen Sea (West Antarctica) and is associated with a... -
Clay mineralogy and shear strength of subglacial and glaciomarine sediments i...
The Belgica Trough and the adjacent Belgica Trough Mouth Fan in the southern Bellingshausen Sea (Pacific sector of the Southern Ocean) mark the location of a major outlet for... -
Sedimentology of various cores from the West Antarctic continental margin
Three megascopic and disseminated tephra layers (which we refer to as layers A, B, and C) occur in late Quaternary glaciomarine sediments deposited on the West Antarctic...