Magnetic susceptibility of sediment core SED-16 from the Antarctic Peninsula Pacific margin
| Cobertura |
LATITUDE: -66.697500 * LONGITUDE: -79.160000 * DATE/TIME START: 1997-03-05T03:12:00 * DATE/TIME END: 1997-03-05T03:12:00 * MINIMUM DEPTH, sediment/rock: 0.06 m * MAXIMUM DEPTH, sediment/rock: 6.31 m |
|---|---|
| Data(s) |
05/12/2007
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| Formato |
text/tab-separated-values, 615 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.671559 doi:10.1594/PANGAEA.671559 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.671563 Lucchi, Renata G; Rebesco, Michele; Camerlenghi, Angelo; Busetti, M; Tomadin, Luciano; Villa, Giuliana; Persico, Davide; Morigi, Caterina; Bonci, MC; Giorgetti, G (2002): Mid-late Pleistocene glacimarine sedimentary processes of a high-latitude, deep-sea sediment drift (Antarctic Peninsula Pacific margin). Marine Geology, 189(3-4), 343-370, doi:10.1016/S0025-3227(02)00470-X |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Bartington MS2B bulk sensor; DEPTH, sediment/rock; Explorer; GC; Gravity corer; SED-16; SEDANO-II; Susceptibility, volume |
| Tipo |
Dataset |
