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Fig. 8. Cyclostratigraphy for late mid-Eocene time from ODP Site 1051. The colour cycle has been assigned an age scale based on magnetic polarity datum points and detrended with a 50 point moving average (right panel) to draw out the high-frequency cycle periods. Spectral analysis of the resulting detrended record is shown below and suggests that the main cycles correspond approximately to the precession bands.

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