4.5. Anisotropy of magnetic susceptibility of SLW1 sediment cores
| Cobertura |
LATITUDE: -82.375000 * LONGITUDE: -168.625000 * MINIMUM DEPTH, sediment/rock: 0.01 m * MAXIMUM DEPTH, sediment/rock: 0.82 m |
|---|---|
| Data(s) |
27/04/2016
|
| Formato |
text/tab-separated-values, 351 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.859983 doi:10.1594/PANGAEA.859983 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.859990 Hodson, Timothy O; Powell, Ross; Brachfield, Stefanie; Tulaczyk, Slawek; Scherer, Reed P; WISSARD Science Team (2016): Physical processes in Subglacial Lake Whillans, West Antarctica: inferences from sediment cores. Earth and Planetary Science Letters, 444, 56-63, doi:10.1016/j.epsl.2016.03.036 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Declination of principle axis K1; Declination of principle axis K2; Declination of principle axis K3; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; Inclination of principle axis K1; Inclination of principle axis K2; Inclination of principle axis K3; Kappabridge, AGICO KLY-4; Magnetic susceptibility; MUC; MultiCorer; PC; PCOR; Percussion corer; Piston corer; Principle axes K1 of normalized anisotropy tensor; Principle axes K2 of normalized anisotropy tensor; Principle axes K3 of normalized anisotropy tensor; SLW1_PC1; SLW1_PEC1; SLW1_SLW_MC1A; SLW1_SLW_MC3A |
| Tipo |
Dataset |
