Table 17. Inclinations from principal component analysis of discrete samples from ODP Site 999.
Sample ID
|
Depth (mbsf)
|
Inclination
(°) |
MAD
|
Type
|
Paleolatitude
|
|---|---|---|---|---|---|
| 165-0999A-001H-2, 63 cm | 2.13 | 24.30 | 9.39 | FRE | 12.72 |
| 165-0999A-001H-3, 63 cm | 3.63 | 19.10 | 7.47 | FRE | 9.82 |
| 165-0999A-001H-5, 63 cm | 6.63 | 21.70 | 9.71 | FRE | 11.25 |
| 165-0999A-003H-4, 63 cm | 22.23 | 25.10 | 5.11 | FRE | 13.18 |
| 165-0999A-003H-5, 3 cm | 23.13 | 19.90 | 3.48 | FRE | 10.26 |
| 165-0999A-004H-3, 63 cm | 30.23 | -13.90 | 8.90 | ANC | 6.90 |
| 165-0999A-004H-4, 63 cm | 31.73 | -24.90 | 1.44 | FRE | 13.07 |
| 165-0999A-004H-5, 63 cm | 33.23 | -39.30 | 1.23 | FRE | 22.26 |
| 165-0999A-004H-6, 63 cm | 34.73 | -36.40 | 5.11 | FRE | 20.24 |
| 165-0999A-004H-7, 63 cm | 36.23 | 39.90 | 5.02 | FRE | 22.69 |
Notes: Inclinations are estimated from principal component analysis (PCA); MAD = maximum angular deviation from the principal component analysis (Kirschvink, 1980); Type = description of the type of line fitted through the demagnetization data in the PCA, where FRE = a line fit through the data only, ANC = a line fit through the data, but anchored to the origin of the demagnetization plot, and BRU = PCA results provided by Bruno Galbrun, used by V. Louvel and B. Galbrun (unpubl. data).
Only a portion of this table appears here. The complete table is available in ASCII.