(Supp. Fig.) Shear strength of sediment core PS2543-1


Autoria(s): Hillenbrand, Claus-Dieter; Ehrmann, Werner; Larter, Robert D; Benetti, Sara; Dowdeswell, Julian A; Cofaigh, Colm Ó; Graham, Alastair GC; Grobe, Hannes
Cobertura

LATITUDE: -70.946667 * LONGITUDE: -89.343333 * DATE/TIME START: 1994-02-18T00:00:00 * DATE/TIME END: 1994-02-18T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.30 m * MAXIMUM DEPTH, sediment/rock: 1.68 m

Data(s)

12/01/2009

Formato

text/tab-separated-values, 22 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.711093

doi:10.1594/PANGAEA.711093

Idioma(s)

en

Publicador

PANGAEA

Relação

doi:10.1594/PANGAEA.711173

Hillenbrand, Claus-Dieter; Ehrmann, Werner; Larter, Robert D; Benetti, Sara; Dowdeswell, Julian A; Cofaigh, Colm Ó; Graham, Alastair GC; Grobe, Hannes (2009): Clay mineral provenance of sediments in the southern Bellingshausen Sea reveals drainage changes of the West Antarctic Ice Sheet during the Late Quaternary. Marine Geology, 265(1-2), 1-18, doi:10.1016/j.margeo.2009.06.009

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Palavras-Chave #ANT-XI/3; AWI_Paleo; Bellingshausen Sea; DEPTH, sediment/rock; Gravity corer (Kiel type); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2543-1; PS29; PS29/051; Rotovisco, Haake; Shear strength, primary; SL
Tipo

Dataset