Magnetism and Opaque Mineralogy of Basalts from the Mid-Atlantic Ridge at 45° N
- 1 December 1970
- journal article
- Published by Springer Nature in Nature
- Vol. 228 (5275), 974-976
- https://doi.org/10.1038/228974a0
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.Keywords
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