Figure F33. Variation in magnetic inclination with depth for the brown claystone in Core 192-1187A-2R and suggested correlation of the interpreted magnetic polarities with the geomagnetic polarity timescale (GPTS). ISEA is alternative name of reversed interval M''-1r'' (e.g., Tarduno et al., 1989) from the site code (Italy, Sentino stream, Site A) used by VandenBerg et al. (1978) in the initial recognition of this subchron.

Figure F33. Variation in magnetic inclination with depth for the brown claystone in Core 192-1187A-2R and suggested correlation of the interpreted magnetic polarities with the geomagnetic polarity timescale (GPTS). ISEA is alternative name of reversed interval M''-1r'' (e.g., Tarduno et al., 1989) from the site code (Italy, Sentino stream, Site A) used by VandenBerg et al. (1978) in the initial recognition of this subchron.