(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 GeoB8601-3
Cobertura |
LATITUDE: 30.848333 * LONGITUDE: -10.268333 * DATE/TIME START: 2003-05-16T20:53:00 * DATE/TIME END: 2003-05-16T20:53:00 * MINIMUM DEPTH, sediment/rock: 0.05 m * MAXIMUM DEPTH, sediment/rock: 4.45 m |
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Data(s) |
25/02/2010
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Formato |
text/tab-separated-values, 688 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.734133 doi:10.1594/PANGAEA.734133 |
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 | #261; 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; GeoB8601-3; Gravity corer (Kiel type); M58/2; MARUM; Meteor (1986); Natural remanent magnetization; NRM, median destructive field of natural remanent magnetisation, alternating field; off Northwest Africa; Saturation isothermal remanent magnetization; Saturation isothermal remanent magnetization, median destructive fields; see reference(s); SL |
Tipo |
Dataset |