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Magnetic remanence was measured on discrete samples by an Agico JR-6A spinner magnetometer, first as natural remanent magnetization (NRM) and then after demagnetization or remagnetization steps were performed on the samples (e.g., alternating field [AF] demagnetization, thermal demagnetization [TD], or isothermal remanent magnetization [IRM]).
forearc, Tsunami, Andaman-Nicobar Islands, megathrust, Ninetyeast Ridge, décollement, Himalaya, shallow seismogenic slip, Nicobar Fan, Indo-Australian plate, Wharton Basin, Expedition 362, JOIDES Resolution, Sunda subduction zone, Sumatra-Andaman 2004 earthquake, Sumatra subduction zone, Bengal Fan, Earthquakes, Site U1480, Site U1481, Indian Ocean
forearc, Tsunami, Andaman-Nicobar Islands, megathrust, Ninetyeast Ridge, décollement, Himalaya, shallow seismogenic slip, Nicobar Fan, Indo-Australian plate, Wharton Basin, Expedition 362, JOIDES Resolution, Sunda subduction zone, Sumatra-Andaman 2004 earthquake, Sumatra subduction zone, Bengal Fan, Earthquakes, Site U1480, Site U1481, Indian Ocean
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