Magnetic polarity structure of the lower oceanic crust

Physics – Geophysics

Scientific paper

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Geomagnetism And Paleomagnetism, Marine Geology And Geophysics: Geomagnetism, Seismology: Oceanic Crust

Scientific paper

A newly developed rock drill was used to take the first fully oriented samples from in-situ gabbros exposed on Atlantis Bank, which formed 11 m.y. ago on the Southwest Indian Ridge (SWIR). These paleomagnetic data locate the seabed outcrop of a normal polarity magnetic lineation within an outcrop of lower crust that correlates with overlying deeptowed and sea-surface magnetic field measurements. A systematic lateral offset between the seabed boundary and measured anomalies implies that the reversal boundary dips ~25° to the south, away from the ridge axis. Paleomagnetic results suggest that following magnetization acquisition, the platform tilted south by ~20° (range: 33 south° to 7° north), implying an original reversal boundary dip of only ~5°.

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