(Fig. 3k) Clay mineral content of sediment core JR104-GC381


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: -69.721667 * LONGITUDE: -83.698333 * DATE/TIME START: 2004-02-08T04:21:00 * DATE/TIME END: 2004-02-08T04:21:00 * MINIMUM DEPTH, sediment/rock: 0.025 m * MAXIMUM DEPTH, sediment/rock: 1.045 m

Data(s)

13/01/2009

Formato

text/tab-separated-values, 44 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.711165

doi:10.1594/PANGAEA.711165

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, steep slope east of TMF; Chlorite; DEPTH, sediment/rock; GC; GC381 CORE_NO 381; Gravity corer; Illite; James Clark Ross; JR104; JR104-GC381; JR20040123; Kaolinite; Smectite; X-ray diffraction (XRD)
Tipo

Dataset