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- W2506736854 abstract "The polarity of the remanent magnetization of hydraulically piston-cored sediments from Hole 512 has been determined. The polarity reversal patterns are correlated to the magnetic reversal time scale, using the initial onboard biostratigraphic reports as a guide for correlation. The upper (middle-upper Miocene) section from 1 to 20 meters sub-bottom depth is correlated to early Chron 10 to late Chron 11 (11.3-11.8 Ma). The lower section (middle Eocene) from 20 to 76 meters sub-bottom depth is correlated to the time scale from Magnetic Anomaly 18 to slightly younger than Magnetic Anomaly 20 (40.9-43.7 Ma). Sedimentation rates for the upper and lower sections are 1.0 cm/1000 y. and 1.7 cm/1000 y., respectively." @default.
- W2506736854 created "2016-08-23" @default.
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- W2506736854 date "2006-01-01" @default.
- W2506736854 modified "2023-09-24" @default.
- W2506736854 title "43. MAGNETOSTRATIGRAPHY OF MIDDLE-UPPER MIOCENE AND UPPER MIDDLE EOCENE SECTIONS IN HOLE 512" @default.
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