(Fig. 3d) Clay mineral content of sediment core JR104-GC357
| Cobertura |
LATITUDE: -71.766700 * LONGITUDE: -80.110000 * DATE/TIME START: 2004-01-31T04:58:00 * DATE/TIME END: 2004-01-31T04:58:00 * MINIMUM DEPTH, sediment/rock: 0.02 m * MAXIMUM DEPTH, sediment/rock: 1.00 m |
|---|---|
| Data(s) |
13/01/2009
|
| Formato |
text/tab-separated-values, 52 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.711151 doi:10.1594/PANGAEA.711151 |
| 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, till sheet on shelf N of Smyley Island; Chlorite; DEPTH, sediment/rock; GC; GC357 CORE_NO 357; Gravity corer; Illite; James Clark Ross; JR104; JR104-GC357; JR20040123; Kaolinite; Smectite; X-ray diffraction (XRD) |
| Tipo |
Dataset |
