(Fig. 3a) Clay mineral content of sediment core JR104-GC366
| Cobertura |
LATITUDE: -72.845000 * LONGITUDE: -82.615000 * DATE/TIME START: 2004-02-03T01:18:00 * DATE/TIME END: 2004-02-03T01:18:00 * MINIMUM DEPTH, sediment/rock: 0.03 m * MAXIMUM DEPTH, sediment/rock: 1.35 m |
|---|---|
| Data(s) |
13/01/2009
|
| Formato |
text/tab-separated-values, 56 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.711157 doi:10.1594/PANGAEA.711157 |
| 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, shallow part of trough in Eltanin Bay; Chlorite; DEPTH, sediment/rock; GC; GC366 CORE_NO 366; Gravity corer; Illite; James Clark Ross; JR104; JR104-GC366; JR20040123; Kaolinite; Smectite; X-ray diffraction (XRD) |
| Tipo |
Dataset |
