10.1594/PANGAEA.971990Stevenard, NathanNathanStevenard0000-0002-1838-9291Université Grenoble Alpes, CNRS, Institut des Géosciences de l'Environnement (IGE), Grenoble, FranceKissel, CatherineCatherineKisselLaboratoire des Sciences du Climat et de l'EnvironnementUniversité Paris-SaclayGovin, AlineAlineGovin0000-0001-8512-5571Laboratoire des Sciences du Climat et de l'EnvironnementUniversité Paris-SaclayWandres, CamilleCamilleWandresLaboratoire des Sciences du Climat et de l'EnvironnementUniversité Paris-SaclayPANGAEA2024Deep current intensitymagnetismNorth Atlantic circulationEvent labelDEPTH, sediment/rockAGEMagnetic susceptibility, low-fieldAnhysteretic remanent magnetizationAnhysteretic remanent magnetization/isothermal remanent magnetization ratioRemanent magnetization, normalized/magnetic susceptibility, low-field, ratioRemanent magnetization, normalized/anhysteretic remanent magnetization ratioRemanent magnetization, normalized/isothermal remanent magnetization ratioPrincipal component analysis inclinationMean angular deviationGeocentric axial dipole field inclinationCalypso CorerBartington MS2 magnetic susceptibility meterMagnetometer [U-channel], 2G Enterprises, Model 755RMD132Marion Dufresne (1995)2003-06-16T10:58:00Dataset10.1594/PANGAEA.97191710.1016/j.quascirev.2024.10901114951 data pointstext/tab-separated-valuesCreative Commons Attribution 4.0 InternationalThe low-field magnetic susceptibility was measured on u-channels using a 45 mm inner diameter Bartington coil.
NRM, IRM and ARM were measured on u-channels using 755R DC-SQUIDS cryogenic magnetometers from 2G Enterprise and demagnetized with 12 steps.-27.814356.3652Gardar Drift