(Figs. 4, 5 and 6) Saturation remanent magnetization (SIRM), anhysteretic remanent magnetization (ARM), natural remanent magnetization (NRM), ARM/NRM ratio and ARM/SIRM ratio of sediment core GeoB6007-2
| Cobertura |
LATITUDE: 30.850000 * LONGITUDE: -10.268300 * DATE/TIME START: 1999-10-18T15:50:00 * DATE/TIME END: 1999-10-18T15:50:00 * MINIMUM DEPTH, sediment/rock: 0.055 m * MAXIMUM DEPTH, sediment/rock: 4.610 m |
|---|---|
| Data(s) |
25/02/2010
|
| Formato |
text/tab-separated-values, 720 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.734098 doi:10.1594/PANGAEA.734098 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.734344 Bleil, Ulrich; Dillon, Melanie (2008): Holocene Earth's magnetic field variations recorded in marine sediments of the NW African continental margin. Studia Geophysica et Geodaetica, 52(2), 133-155, doi:10.1007/s11200-008-0010-6 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #AGE; Anhysteretic remanent magnetization; Anhysteretic remanent magnetization/natural remanent magnetization ratio; Anhysteretic remanent magnetization/saturation isothermal remanent magnetization ratio; ARM, median destructive field of anhysteretic remanent magnetisation; Calculated, see reference(s); Center for Marine Environmental Sciences; DEPTH, sediment/rock; GeoB6007-2; Gravity corer (Kiel type); M45/5a; MARUM; Meteor (1986); Natural remanent magnetization; NRM, median destructive field of natural remanent magnetisation, alternating field; Saturation isothermal remanent magnetization; Saturation isothermal remanent magnetization, median destructive fields; see reference(s); SL |
| Tipo |
Dataset |
