Volume magnetic susceptibility of sediments from the Ioffe Drift (South Atlantic)

The magnetic susceptibility was measured on split-cores using the MSCL XYZ core workstation (Bartington MS3 system with Bartington MS2E sensor. Split-cores were covered with Chemplex Prolene 416 film - 4.0μm. step (downcore resolution): 0.5 cm; measurement time - 1 second; zero (in air) measurment - after each sample measurement; The location, depth and length of the studied cores are given in List_of_cores_MS.xlsx