Table 18. Inclinations from principal component analysis of discrete samples from ODP Site 1001.
Sample ID
|
Depth (mbsf)
|
Inclination
(°) |
MAD
|
Type
|
Paleolatitude
|
|---|---|---|---|---|---|
| Sedimentary samples | |||||
| 165-1001A-018R-1, 14 cm | 160.43 | 42.00 | 9.99 | BRU | 24.24 |
| 165-1001A-018R-2, 17 cm | 161.96 | 40.50 | 9.99 | BRU | 23.12 |
| 165-1001A-018R-3, 19 cm | 163.48 | -3.60 | 9.99 | BRU | 1.80 |
| 165-1001A-018R-4, 63 cm | 165.42 | -1.00 | 9.99 | BRU | 0.50 |
| 165-1001A-020R-1, 54 cm | 170.53 | -2.70 | 9.99 | BRU | 1.35 |
| 165-1001A-021R-1, 42 cm | 180.01 | -9.70 | 9.99 | BRU | 4.89 |
| 165-1001A-023R-1, 85 cm | 199.64 | 15.20 | 9.99 | BRU | 7.74 |
| 165-1001A-024R-1, 46 cm | 208.85 | -4.50 | 9.99 | BRU | 2.25 |
| 165-1001A-024R-1, 82 cm | 209.22 | -14.30 | 4.30 | ANC | 7.26 |
| 165-1001A-024R-2, 21 cm | 210.10 | 3.60 | 9.99 | BRU | 1.80 |
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.