Table 16. Inclinations from principal component analysis of discrete samples from ODP Site 998.
Sample ID
|
Depth
(mbsf) |
Inclination
(°) |
MAD
|
Type
|
Paleolatitude
|
---|---|---|---|---|---|
165-0998A-001H-5, 61 cm | 6.61 | 37.70 | 2.88 | FRE | 21.13 |
165-0998A-001H-6, 61 cm | 8.11 | 48.70 | 5.44 | FRE | 29.65 |
165-0998A-002H-2, 61 cm | 10.91 | 55.40 | 7.41 | FRE | 35.93 |
165-0998A-002H-4, 11 cm | 13.41 | 38.10 | 9.28 | FRE | 21.41 |
165-0998A-002H-4, 61 cm | 13.91 | 46.70 | 9.32 | FRE | 27.95 |
165-0998A-002H-5, 61 cm | 15.41 | 37.70 | 6.98 | FRE | 21.13 |
165-0998A-002H-6, 61 cm | 16.91 | 28.90 | 7.71 | FRE | 15.43 |
165-0998A-003H-5, 61 cm | 24.91 | 30.10 | 9.37 | FRE | 16.16 |
165-0998A-004H-5, 61 cm | 34.41 | -21.90 | 4.43 | FRE | 11.36 |
165-0998A-008H-3, 61 cm | 69.41 | 21.90 | 1.78 | FRE | 11.36 |
Notes: Inclinations are estimated from principal component inclination analysis (PCA). MAD = maximum angular deviation from the demagnetization data in the PCA (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.