Figure F22. Declination of magnetic remanence after applying orientation using the FlexIt tool and 20 mT peak alternating-field demagnetization. Interpretations are hampered by weak magnetization intensities and scattered directional data in some intervals. Core composite depths below seafloor were determined independent of the polarity record. See Table T16. GPTS = geomagnetic polarity timescale. A. 0–110 m CCSF-A. (Continued on next page.)
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