
Magnetic remanence was measured on section halves (and rarely on whole-round sections) using a 2G Enterprises 760R cryogenic magnetometer, first as natural remanent magnetization (NRM) and then after demagnetization steps were performed on the samples by alternating field (AF) demagnetizer coils mounted in-line within the instrument.
Expedition 360, Mohorovicic discontinuity, International Ocean Discovery Program, Moho, mid-ocean ridge, Atlantis II Transform, Southwest Indian Ridge, Hole 1105A, IODP, JOIDES Resolution, slow spreading ridge, upper mantle, Atlantis Bank, Earth connections, SloMo, Site U1473
Expedition 360, Mohorovicic discontinuity, International Ocean Discovery Program, Moho, mid-ocean ridge, Atlantis II Transform, Southwest Indian Ridge, Hole 1105A, IODP, JOIDES Resolution, slow spreading ridge, upper mantle, Atlantis Bank, Earth connections, SloMo, Site U1473
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