Paleomagnetic analysis of sediment core GeoB5112-4
| Cobertura |
LATITUDE: -23.825000 * LONGITUDE: -16.258333 * DATE/TIME START: 1998-04-29T16:32:00 * DATE/TIME END: 1998-04-29T16:32:00 * MINIMUM DEPTH, sediment/rock: -0.35 m * MAXIMUM DEPTH, sediment/rock: 5.55 m |
|---|---|
| Data(s) |
24/11/2004
|
| Formato |
text/tab-separated-values, 122 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.219501 doi:10.1594/PANGAEA.219501 |
| 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 | #06MT41_3; Brazil Basin; ChRM, Declination; ChRM, Inclination; DEPTH, sediment/rock; GeoB; GeoB5112-4; Geosciences, University of Bremen; Gravity corer (Kiel type); M41/3; Meteor (1986); SFB261; Single sample demagnetization; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents |
| Tipo |
Dataset |
