Susceptibility versus depth and age of sediment core GeoB6426-1


Autoria(s): Schmieder, Frank
Cobertura

LATITUDE: -33.499200 * LONGITUDE: -24.024200 * DATE/TIME START: 2000-03-02T15:41:00 * DATE/TIME END: 2000-03-02T15:41:00 * MINIMUM DEPTH, sediment/rock: 0.01 m * MAXIMUM DEPTH, sediment/rock: 13.30 m

Data(s)

25/11/2004

Formato

text/tab-separated-values, 1309 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.219637

doi:10.1594/PANGAEA.219637

Idioma(s)

en

Publicador

PANGAEA

Relação

Schmieder, Frank (2004): Magnetic signals in Plio-Pleistocene sediments of the South Atlantic: Chronostratigraphic usability and paleooceanographic implications. In: Wefer, G; Mulitza, S & Ratmeyer, V (eds.), The South Atlantic in the Late Quaternary: Reconstruction of Material Budgets and Current Systems, Springer, Berlin, Heidelberg, New York, 261-277, doi:10.1007/978-3-642-18917-3_13

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Palavras-Chave #AGE; Bartington MS2F spot sensor; DEPTH, sediment/rock; GeoB; GeoB6426-1; Geosciences, University of Bremen; Gravity corer (Kiel type); M46/4; Meteor (1986); SFB261; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents; Susceptibility, volume
Tipo

Dataset