(Fig. 15a) Hysteresis loops to maximum fields of 0.3 T for samples from sediment core GeoB1713-5
| Cobertura |
LATITUDE: -23.216667 * LONGITUDE: 13.011667 * DATE/TIME START: 1992-01-12T00:00:00 * DATE/TIME END: 1992-01-12T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.02 m * MAXIMUM DEPTH, sediment/rock: 0.15 m |
|---|---|
| Data(s) |
01/03/1999
|
| Formato |
text/tab-separated-values, 6038 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.776847 doi:10.1594/PANGAEA.776847 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
Frederichs, Thomas; Bleil, Ulrich; Däumler, Katharina; von Dobeneck, Tilo; Schmidt, Andrea (1999): The Magnetic View on the Marine Paleoenvironment: Parameters, Techniques, and Potentials of Rock Magnetic Studies as a Key to Paleoclimatic and Paleoceanographic Changes. In: Fischer, G & Wefer, G (eds.), Use of Proxies in Paleoceanography - Examples from the South Atlantic, Springer, Berlin, Heidelberg, 575-599 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #DEPTH, sediment/rock; GeoB; GeoB1713-5; Geosciences, University of Bremen; M20/2; Magnetic field, hysteresis; Meteor (1986); MUC; MultiCorer; Namibia continental slope; SFB261; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents; Specific saturation magnetization |
| Tipo |
Dataset |
