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