(Supp. Fig.) Clay mineral content of sediment core PS2540-3


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: -70.065000 * LONGITUDE: -87.923333 * DATE/TIME START: 1994-02-17T13:15:00 * DATE/TIME END: 1994-02-17T13:15:00 * MINIMUM DEPTH, sediment/rock: 0.015 m * MAXIMUM DEPTH, sediment/rock: 4.050 m

Data(s)

13/01/2009

Formato

text/tab-separated-values, 164 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.711168

doi:10.1594/PANGAEA.711168

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; Chlorite; DEPTH, sediment/rock; Gravity corer (Kiel type); Illite; Kaolinite; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2540-3; PS29; PS29/048; SL; Smectite; X-ray diffraction TEXTUR, clay fraction
Tipo

Dataset