4.5. Principal Component Analysis calculation of best fit line for multiple demagnetization steps in order to determine the inclination and declination of SLW1 sediment cores
| Cobertura |
LATITUDE: -82.375000 * LONGITUDE: -168.625000 * MINIMUM DEPTH, sediment/rock: 0.14 m * MAXIMUM DEPTH, sediment/rock: 0.56 m |
|---|---|
| Data(s) |
27/04/2016
|
| Formato |
text/tab-separated-values, 28 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.859984 doi:10.1594/PANGAEA.859984 |
| 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 | #Demagnetization step; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; Maximum angular deviation; MUC; MultiCorer; NRM, Declination after demagnetisation; NRM, Inclination after demagnetisation; PC; Piston corer; Principal component analyses (PCA); SLW1_PC1; SLW1_SLW_MC3A |
| Tipo |
Dataset |
