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Kinoshita, Hajimu; Furuta, Toshio; Kawahata, Hodaka (1985): (Table 1) Paleomagnetism at DSDP Hole 83-504B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.805114, In supplement to: Kinoshita, H et al. (1985): Magnetic properties and alteration in basalt, Hole 504B, Deep Sea Drilling Project Leg 83. In: Anderson, RN; Honnorez, J; Becker, K; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 83, 331-338, https://doi.org/10.2973/dsdp.proc.83.116.1985

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Project(s):
Coverage:
Latitude: 1.227200 * Longitude: -83.730200
Date/Time Start: 1981-11-22T00:00:00 * Date/Time End: 1982-01-02T00:00:00
Minimum DEPTH, sediment/rock: 837.28 m * Maximum DEPTH, sediment/rock: 1332.29 m
Event(s):
83-504B * Latitude: 1.227200 * Longitude: -83.730200 * Date/Time Start: 1981-11-22T00:00:00 * Date/Time End: 1982-01-02T00:00:00 * Elevation: -3460.0 m * Penetration: 1350 m * Recovery: 107.7 m * Campaign: Leg83 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: Leg 83 of DSDP was devoted entirely to coring and experiments in Hole 504B, the deepest borehole to date into the oceanic crust. Hole 504B now extends over a kilometer into basement, nearly twice as far as any other DSDP hole, and it is the only DSDP hole to have clearly penetrated into the intrusive sheeted dikes that underlie the extrusive pillow lavas of the upper oceanic crust. At Hole 504B, Leg 83 continued an ongoing DSDP effort that began during Legs 68, 69, and 70 in 1979, and also included part of Leg 92 in 1983. 71 cores; 514 m cored; 0 m drilled; 21 % recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Sample code/labelSample labelKinoshita, HajimuDSDP/ODP/IODP sample designation
2DEPTH, sediment/rockDepth sedmGeocode – mbsf
3NRM, IntensityInten (NRM)mA/mKinoshita, Hajimusee reference(s)
4NRM, Inclination after demagnetizationIncl (AF)degKinoshita, Hajimusee reference(s)
5Susceptibility, volumekappaµGs/OeKinoshita, Hajimusee reference(s)
6Koenigsberger ratioQ-ratioOeKinoshita, Hajimusee reference(s)
7Median demagnetizing fieldMDFOeKinoshita, Hajimusee reference(s)
8Specific saturation magnetizationIsmA*m2/kgKinoshita, Hajimusee reference(s)
9UnitUnitKinoshita, Hajimusee reference(s)Magnetic unit based on stable inclination
Size:
490 data points

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