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

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NIAID Data Ecosystem2026-03-13 收录
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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
创建时间:
2022-06-01
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