Magnetism and opaque mineralogy of basalts from the Mid-Atlantic Ridge at 45 degrees N.
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.
Irving
E
E
Department of Energy, Mines and Resources, Ottawa.
Park
J K
JK
Haggerty
S E
SE
Aumento
F
F
Loncarevic
B
B