Documentation of sediment core JR104-GC362
| Cobertura |
LATITUDE: -72.596700 * LONGITUDE: -80.830000 * DATE/TIME START: 2004-02-02T00:00:00 * DATE/TIME END: 2004-02-02T00:00:00 * MINIMUM ELEVATION: -845.0 m * MAXIMUM ELEVATION: -845.0 m |
|---|---|
| Data(s) |
04/06/2009
|
| Formato |
, unknown |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.717162 doi:10.1594/PANGAEA.717162 |
| 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, part of trough exiting Carroll Inlet; MSGL/drumlins trend 335¡; GC; GC362 CORE_NO 362; Gravity corer; James Clark Ross; JR104; JR104-GC362; JR20040123 |
| Tipo |
Dataset |
