Magnetic susceptibility of sediment core SED-11 from the Antarctic Peninsula Pacific margin
Cobertura |
LATITUDE: -67.143500 * LONGITUDE: -76.368167 * DATE/TIME START: 1997-03-02T19:09:00 * DATE/TIME END: 1997-03-02T19:09:00 * MINIMUM DEPTH, sediment/rock: 0.02 m * MAXIMUM DEPTH, sediment/rock: 5.01 m |
---|---|
Data(s) |
05/12/2007
|
Formato |
text/tab-separated-values, 461 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.671556 doi:10.1594/PANGAEA.671556 |
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-11; SEDANO-II; Susceptibility, volume |
Tipo |
Dataset |