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Chen, Quan; Kissel, Catherine; Liu, Zhifei (2017): High-resolution magnetic properties obtained by scanning U-channel samples of sediment core MD12-3432 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.874820, In supplement to: Chen, Q et al. (2017): Late Quaternary climatic forcing on the terrigenous supply in the northern South China Sea: Input from magnetic studies. Earth and Planetary Science Letters, 471, 160-171, https://doi.org/10.1016/j.epsl.2017.04.047

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Coverage:
Latitude: 19.281330 * Longitude: 116.242000
Minimum DEPTH, sediment/rock: 0.07 m * Maximum DEPTH, sediment/rock: 50.75 m
Event(s):
MD12-3432 * Latitude: 19.281330 * Longitude: 116.242000 * Elevation: -2125.0 m * Recovery: 50.8 m * Location: South China Sea * Campaign: MD190 (CIRCEA) * Basis: Marion Dufresne (1995) * Method/Device: Calypso Corer (CALYPSO)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepth sedmKissel, CatherineGeocode
2AGEAgeka BPKissel, CatherineGeocode
3Magnetic susceptibility, high-fieldKHF10-6 SIKissel, Catherinecorrected for the dilution by carbonate content
4ARM, Intensity, per unit volumeInten (ARM)mA/mKissel, Catherineobtained applying AF peak field of 100 mT and DC field of 50µT, translation speed 1cm/s
5IRM, Intensity, per unit volumeInten (IRM)mA/mKissel, CatherineIRM IT = obtained at 1T using a 1.6 m long solenoid
6IRM, Intensity, per unit volumeInten (IRM)mA/mKissel, CatherineIRM Af@80mT = remaining after alternating field demagnetization at 80 mT expressed as % of the initial IRM1T
7S-ratio (hematite/magnetite)S-rKissel, CatherineS-ratio 0.3T = ratio between the inverse of the magnetization obtained applying a back field of 0.3T and the IRM1T
8Hard isothermal remanent magnetizationHIRMmA/mKissel, Catherinehalf sum of the inverse of the magnetization obtained applying a back field of 0.3T and the IRM1T
Size:
13902 data points

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