Figure F46. Characteristic remanent magnetization inclination values from Hole U1301B igneous samples. Dashed vertical lines show expected geocentric axial dipole inclination for the site (64° = normal polarity; –64° = reversed polarity), corrected for bias expected from averaging azimuthally unoriented samples (Cox and Gordon, 1984). Open circles = thermally demagnetized samples, solid symbols = samples that were demagnetized with the AF method. Solid circles = standard paleomagnetic cube samples, solid diamonds = measurements from archive-half core pieces, solid triangles = samples that were taken by physical property scientists for velocity measurements. Column at left shows core depths and recovery, with the numbers being the core numbers. Horizontal ticks on the 0° axis at the middle of the plot show the stratigraphic positions of samples that produced results deemed to be unreliable, with one tick per sample.
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