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Measurements of the anisotropy of magnetic susceptibility (AMS) in basalt cores between 125 and 130 meters depth at Site 321 reveal a consistently near-horizontal direction of minimum susceptibility, with the directions of intermediate and maximum susceptibility confined to a vertical plane. Together with a low stability of remanent magnetism, this is indicative of an intrusive origin. In contrast, basalt between 90 and 150 meters depth in Hole 319A possesses highly variable AMS directions and remanent magnetism stability, showing the presence of several different bodies of probably mixed emplacement mode.

Diagnosis of Emplacement Mode of Basalt in Hole 319A and Site 321