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Acton, Gary D; Guyodo, Yohan; Brachfeld, Stefanie A (2002): (Table T10) Principal component analysis results from U-channel paleomagnetic data, ODP Hole 178-1095A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.737895, In supplement to: Acton, GD et al. (2002): Magnetostratigraphy of sediment drifts on the continental rise of West Antarctica (ODP Leg 178, Sites 1095, 1096, and 1101). In: Barker, PF; Camerlenghi, A; Acton, GD; Ramsay, ATS (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 178, 1-61, https://doi.org/10.2973/odp.proc.sr.178.235.2002

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Project(s):
Coverage:
Latitude: -66.985450 * Longitude: -78.487310
Date/Time Start: 1998-02-17T16:15:00 * Date/Time End: 1998-02-18T19:30:00
Minimum DEPTH, sediment/rock: 0.06 m * Maximum DEPTH, sediment/rock: 19.95 m
Event(s):
178-1095A * Latitude: -66.985450 * Longitude: -78.487310 * Date/Time Start: 1998-02-17T16:15:00 * Date/Time End: 1998-02-18T19:30:00 * Elevation: -3841.6 m * Penetration: 87.3 m * Recovery: 86.48 m * Location: South Pacific Ocean * Campaign: Leg178 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 10 cores; 87.3 m cored; 0 m drilled; 99.1 % recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Sample code/labelSample labelActon, Gary DDSDP/ODP/IODP sample designation
2DEPTH, sediment/rockDepth sedmGeocode
3Depth, compositeDepth compmcdActon, Gary DIntercore correlation
4NRM, InclinationIncl (NRM)degActon, Gary DPrincipal component analyses (PCA)
5NRM, DeclinationDecl (NRM)degActon, Gary DPrincipal component analyses (PCA)
6Maximum angular deviationMADdegActon, Gary DPrincipal component analyses (PCA)
7--Acton, Gary DPrincipal component analyses (PCA)length (A/m) = distance from origin of the vector demagnetization space to the centroid of the data used to find the best-fit line
8AngleAngledegActon, Gary DPrincipal component analyses (PCA)deviation angle = the angle between the best-fit line and a line that passes through the origin and centroid
9NumberNoActon, Gary DPrincipal component analyses (PCA)number of steps = number of demagnetization steps used in finding the best-fit line
10Demagnetization stepDemag stepmTActon, Gary DPrincipal component analyses (PCA)lowest step = the lowest demagnetization step used in finding the best-fit line
11Demagnetization stepDemag stepmTActon, Gary DPrincipal component analyses (PCA)highest step = the highest demagnetization step used in finding the best-fit line
12NRM, InclinationIncl (NRM)degActon, Gary DFishers method
13NRM, DeclinationDecl (NRM)degActon, Gary DFishers method
14Fisherian dispersion parameterkActon, Gary DFishers method
15NumberNoActon, Gary DFishers methodnumber of directions from the three highest demagnetization steps that were averaged
16Angular distanceAngular distdegActon, Gary Dthe angular distance between the PCA direction and the stable end point direction
Size:
11205 data points

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