(Fig. 3f) Clay mineral content of sediment core JR104-GC371


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: -70.653300 * LONGITUDE: -84.540000 * DATE/TIME START: 2004-02-04T19:28:00 * DATE/TIME END: 2004-02-04T19:28:00 * MINIMUM DEPTH, sediment/rock: 0.01 m * MAXIMUM DEPTH, sediment/rock: 1.89 m

Data(s)

13/01/2009

Formato

text/tab-separated-values, 72 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.711160

doi:10.1594/PANGAEA.711160

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, central axis of trough, outer shelf; Chlorite; DEPTH, sediment/rock; GC; GC371 CORE_NO 371; Gravity corer; Illite; James Clark Ross; JR104; JR104-GC371; JR20040123; Kaolinite; Smectite; X-ray diffraction (XRD)
Tipo

Dataset