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Figure F23. Magnetic susceptibility (top) and relative paleointensity (bottom) plotted against depth (mbsf), Hole U1344A. Relative paleointensity is estimated by normalizing natural remanent magnetization after 20 mT demagnetization (Int20 mT) by magnetic susceptibility. Marine isotope Stages (MIS) 1–19 in the Brunhes Chron, numbered at top, were tentatively identified by correlating these features to other sites.

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