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Thirteen basalt samples have been investigated, eleven of which were oriented with respect to vertical. The natural remanent magnetization, low field susceptibility, a.c. and d.c. field stability, saturation remanence, saturation magnetization, and Curie temperature have been measured. These measurements have been complemented by ore microscopic analysis. The remanence directions of the samples closely group around the magnetic dipole field direction to be expected at the latitude of Hole 373A. In all samples apart from one, cation-deficient titanomagnetite is the main carrier of magnetization. It is concluded that the samples have undergone low temperature oxidation in a submarine environment.

Rock and Paleomagnetism of Leg 42A, Hole 373A Basalts