(Supp. Fig.) Shear strength of sediment core JR104-GC372


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: -70.605000 * LONGITUDE: -86.253300 * DATE/TIME START: 2004-02-05T00:37:00 * DATE/TIME END: 2004-02-05T00:37:00 * MINIMUM DEPTH, sediment/rock: 0.02 m * MAXIMUM DEPTH, sediment/rock: 1.96 m

Data(s)

12/01/2009

Formato

text/tab-separated-values, 20 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.711088

doi:10.1594/PANGAEA.711088

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 #Bellingshausen Sea, toe of eastern bank of mini trough, outer shelf; DEPTH, sediment/rock; GC; GC372 CORE_NO 372; Gravity corer; James Clark Ross; JR104; JR104-GC372; JR20040123; Rotovisco, Haake; Shear strength, primary
Tipo

Dataset