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Magnetism and opaque mineralogy of basalts from the Mid-Atlantic Ridge at 45 degrees N
Authors:Irving E  Park J K  Haggerty S E  Aumento F  Loncarevic B
Affiliation:Department of Energy, Mines and Resources, Ottawa.
Abstract:The volcanic layer may be only 200 m thick at 45 degrees N and oxidation of titanomagnetite may be responsible for the decrease in amplitude of the magnetic anomalies away from the ridge axis.
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