Figure F25. Continuous magnetic inclination and declination record in pelagic sediments at Site 1201 (large dots correspond to discrete samples). Also shown is the best fit to the late Oligocene through late Miocene geomagnetic polarity timescale based on paleontological markers from the site. In the polarity column, black bands = normal and white bands = reversed polarity.

Figure F25. Continuous magnetic inclination and declination record in pelagic sediments at Site 1201 (large dots correspond to discrete samples). Also shown is the best fit to the late Oligocene through late Miocene geomagnetic polarity timescale based on paleontological markers from the site. In the polarity column, black bands = normal and white bands = reversed polarity.