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Wang, Daming; Van der Voo, Rob; Peacor, Donald R (2005): (Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma, DSDP Hole 28-267. PANGAEA,, In supplement to: Wang, D et al. (2005): Why is the remanent magnetic intensity of Cretaceous MORB so much higher than that of mid to late Cenozoic MORB? Geosphere, 1(3), 138-146,

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Latitude: -59.262300 * Longitude: 104.488300
Date/Time Start: 1973-01-06T00:00:00 * Date/Time End: 1973-01-06T00:00:00
Minimum DEPTH, sediment/rock: 204.89 m * Maximum DEPTH, sediment/rock: 211.19 m
28-267 * Latitude: -59.262300 * Longitude: 104.488300 * Date/Time: 1973-01-06T00:00:00 * Elevation: -4522.0 m * Penetration: 219.5 m * Recovery: 26.1 m * Location: Antarctic Ocean/BASIN * Campaign: Leg28 * Basis: Glomar Challenger * Device: Drilling/drill rig (DRILL) * Comment: 6 cores; 48.5 m cored; 9.5 m drilled; 53.8 % recovery
#NameShort NameUnitPrincipal InvestigatorMethodComment
1DEPTH, sediment/rockDepthmGeocode
2AGEAgeka BPGeocode
3Sample code/labelSample labelWang, DamingODP sample designation
4Curie temperatureCurie temp°CWang, Daming
5Hysteresis, saturation magnetization/ saturation remanenceMrs/MsWang, Damingvibrating sample magnetometer (microVSM)
6Hysteresis, coercivity of remanence/coercivityHcr/HcWang, Damingvibrating sample magnetometer (microVSM)
7Hysteresis, saturation remanenceMrsmA m2/kgWang, Damingvibrating sample magnetometer (microVSM)
8CoercivityHcmTWang, Damingvibrating sample magnetometer (microVSM)
9NRM, Intensity per unit massInten (NRM) /mass10-6 A*m2/kgWang, Damingvibrating sample magnetometer (microVSM)
20 data points

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