Figure F14. Inferred paleolatitudes for Sites 1218, 1219, and 1220 based on mean paleomagnetic inclinations, using the dipole formula. Error bars represent the maximum difference obtained from different holes around their mean. Site 1218 has not produced data older than the Oligocene. Notice that Site 1219 crosses the equator much later than Site 1220. Data points at 0 Ma are the present-day latitudes of the studied sites.
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