Magnetic susceptibility of sediment core SED-19 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: -64.227333 * LONGITUDE: -70.836500 * DATE/TIME START: 1997-03-14T19:52:00 * DATE/TIME END: 1997-03-14T19:52:00 * MINIMUM DEPTH, sediment/rock: 0.03 m * MAXIMUM DEPTH, sediment/rock: 6.41 m

Data(s)

05/12/2007

Formato

text/tab-separated-values, 625 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.671562

doi:10.1594/PANGAEA.671562

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-19; SEDANO-II; Susceptibility, volume
Tipo

Dataset