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Data Publisher for Earth & Environmental Science

Galbrun, Bruno (1992): (Appendix D) Directions of characteristic magnetization of Triassic sediments in ODP Hole 122-761C [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.760700, In supplement to: Galbrun, B (1992): Triassic (Upper Carnian-Lower Rhaetian) magnetostratigraphy of Leg 122 sediments, Wombat Plateau, Northwest Australia. In: von Rad, U; Haq, BU; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 122, 685-698, https://doi.org/10.2973/odp.proc.sr.122.150.1992

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Project(s):
Coverage:
Latitude: -16.737000 * Longitude: 115.535000
Date/Time Start: 1988-07-21T09:00:00 * Date/Time End: 1988-07-25T02:00:00
Minimum DEPTH, sediment/rock: 338.66 m * Maximum DEPTH, sediment/rock: 428.91 m
Event(s):
122-761C * Latitude: -16.737000 * Longitude: 115.535000 * Date/Time Start: 1988-07-21T09:00:00 * Date/Time End: 1988-07-25T02:00:00 * Elevation: -2179.0 m * Penetration: 436.7 m * Recovery: 72.24 m * Location: South Indian Ridge, South Indian Ocean * Campaign: Leg122 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 33 cores; 436.7 m cored; 0 m drilled; 16.5 % recovery
Comment:
The NRM column represents the initial NRM intensity of each sample, the demagnetization step column refers to the highest step attained during the treatment of each sample.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Sample code/labelSample labelGalbrun, BrunoDSDP/ODP/IODP sample designation
2DEPTH, sediment/rockDepth sedmGeocode
3NRM, IntensityInten (NRM)mA/mGalbrun, BrunoMagnetometer, cryogenic, pass-through, 2G Enterprises 755 R
4NRM, InclinationIncl (NRM)degGalbrun, BrunoMagnetometer, cryogenic, pass-through, 2G Enterprises 755 R
5Demagnetization levelLevel°CGalbrun, BrunoMagnetometer, cryogenic, pass-through, 2G Enterprises 755 R
6Demagnetization stepDemag stepmTGalbrun, BrunoMagnetometer, cryogenic, pass-through, 2G Enterprises 755 R
Size:
170 data points

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