Magnetic susceptibility of sediment core SED-11 from the Antarctic Peninsula Pacific margin


Autoria(s): Lucchi, Renata G; Rebesco, Michele; Camerlenghi, Angelo; Busetti, M; Tomadin, Luciano; Villa, Giuliana; Persico, Davide; Morigi, Caterina; Bonci, MC; Giorgetti, G
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