Magnetism and Opaque Mineralogy of Basalts from the Mid-Atlantic Ridge at 45° N

Details Magnetism and Opaque Mineralogy of Basalts from the Mid-Atlantic Ridge at 45° N Magnetism and Opaque Mineralogy of Basalts from the Mid-Atlantic Ridge at 45° N

Dec 1970

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1970natur.228..974i&link_type=abstract

Nature, Volume 228, Issue 5275, pp. 974-976 (1970).

Physics

11

Scientific paper

The volcanic layer may be only 200 m thick at 45° 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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