Paleomagnetic analysis of sediment core GeoB6429-2
| Cobertura |
LATITUDE: -31.950000 * LONGITUDE: -24.248200 * DATE/TIME START: 2000-03-04T04:55:00 * DATE/TIME END: 2000-03-04T04:55:00 * MINIMUM DEPTH, sediment/rock: 0.05 m * MAXIMUM DEPTH, sediment/rock: 7.15 m |
|---|---|
| Data(s) |
24/11/2004
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| Formato |
text/tab-separated-values, 286 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.219506 doi:10.1594/PANGAEA.219506 |
| 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 | #ChRM, Declination; ChRM, Inclination; DEPTH, sediment/rock; GeoB; GeoB6429-2; Geosciences, University of Bremen; Gravity corer (Kiel type); M46/4; Meteor (1986); SFB261; Single sample demagnetization; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents |
| Tipo |
Dataset |
