Acton, Gary D; Guyodo, Yohan; Brachfeld, Stefanie A (2002): (Table T12) Principal component analysis results from U-channel paleomagnetic data, ODP Hole 178-1095D [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.737901, 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):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -66.985350 * Longitude: -78.488080
Date/Time Start: 1998-02-24T00:00:00 * Date/Time End: 1998-02-24T00:00:00
Minimum DEPTH, sediment/rock: 0.36 m * Maximum DEPTH, sediment/rock: 27.32 m
Event(s):
178-1095D * Latitude: -66.985350 * Longitude: -78.488080 * Date/Time: 1998-02-24T00:00:00 * Elevation: -3840.9 m * Penetration: 84.6 m * Recovery: 78.96 m * Location: South Pacific Ocean * Campaign: Leg178 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 9 cores; 84.6 m cored; 0 m drilled; 93.3 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Acton, Gary D | DSDP/ODP/IODP sample designation | ||
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 3 | Depth, composite | Depth comp | mcd | Acton, Gary D | Intercore correlation | |
| 4 | NRM, Inclination | Incl (NRM) | deg | Acton, Gary D | Principal component analyses (PCA) | |
| 5 | NRM, Declination | Decl (NRM) | deg | Acton, Gary D | Principal component analyses (PCA) | |
| 6 | Maximum angular deviation | MAD | deg | Acton, Gary D | Principal component analyses (PCA) | |
| 7 | - | - | Acton, Gary D | Principal 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 | |
| 8 | Angle | Angle | deg | Acton, Gary D | Principal component analyses (PCA) | deviation angle = the angle between the best-fit line and a line that passes through the origin and centroid |
| 9 | Number | No | Acton, Gary D | Principal component analyses (PCA) | number of steps = number of demagnetization steps used in finding the best-fit line | |
| 10 | Demagnetization step | Demag step | mT | Acton, Gary D | Principal component analyses (PCA) | lowest step = the lowest demagnetization step used in finding the best-fit line |
| 11 | Demagnetization step | Demag step | mT | Acton, Gary D | Principal component analyses (PCA) | highest step = the highest demagnetization step used in finding the best-fit line |
| 12 | NRM, Inclination | Incl (NRM) | deg | Acton, Gary D | Fishers method | |
| 13 | NRM, Declination | Decl (NRM) | deg | Acton, Gary D | Fishers method | |
| 14 | Fisherian dispersion parameter | k | Acton, Gary D | Fishers method | ||
| 15 | Number | No | Acton, Gary D | Fishers method | number of directions from the three highest demagnetization steps that were averaged | |
| 16 | Angular distance | Angular dist | deg | Acton, Gary D | the angular distance between the PCA direction and the stable end point direction |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
15900 data points
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