Figure F5. Magnetostratigraphic record from Site 1165 for 0-50 mbsf. The paleomagnetic inclination is shown after demagnetization at 20-30 mT for the split cores (solid line) along with characteristic remanent magnetization (ChRM) data for stepwise-demagnetized discrete samples (open squares). Polarity is shown on the log to the right. Black (white) = normal (reversed) polarity. Marine diatom and radiolarian datums are used to constrain the interpretation. The geomagnetic polarity timescale is from Berggren et al. (1995). (see Fig. F3 for data sources)

Figure F5. Magnetostratigraphic record from Site 1165 for 0-50 mbsf. The paleomagnetic inclination is shown after demagnetization at 20-30 mT for the split cores (solid line) along with characteristic remanent magnetization (ChRM) data for stepwise-demagnetized discrete samples (open squares). Polarity is shown on the log to the right. Black (white) = normal (reversed) polarity. Marine diatom and radiolarian datums are used to constrain the interpretation. The geomagnetic polarity timescale is from Berggren et al. (1995). (see Fig. F3 for data sources)