Daftar Isi: IODP Expedition 366 Magnetic susceptibility (section half)

Main Authors:	Fryer, P., Wheat, C.G., Williams, T., Albers, E., Bekins, B., Debret, B.P.R., Deng, J., Dong, Y., Eickenbusch, P., Frery, E.A., Ichiyama, Y., Johnson, K., Johnston, R.M., Kevorkian, R.T., Kurz, W., Magalhaes, V., Mantovanelli, S.S., Menapace, W., Menzies, C.D., Michibayashi, K., Moyer, C.L., Mullane, K.K., Park, J.-W., Price, R.E., Ryan, J.G., Shervais, J.W., Sissmann, O.J., Suzuki, S., Takai, K., Walter, B., Zhang, R.
Other Authors:	International Ocean Discovery Program
Format:	info dataset
Terbitan:	, 2020
Subjects:	Expedition 366 Mariana Site 1200 Site U1491 Site U1492 Site U1493 Site U1494 Site U1495 Site U1496 Site U1497 Site U1498 Leg 195 Deep biosphere subseafloor biosphere Earth in Motion seismic zones JOIDES Resolution Pacific plate Asut Tesoru Seamount Conical Seamount Fantangisna Seamount South Chamorro Seamount Ynazao Seamount Blue Moon Seamount Big Blue Seamount Celestial Seamount subduction seismogenic zone mud volcano serpentinite CORK forearc harzburgite ultramafic rock reef limestone guyot
Online Access:	https://zenodo.org/record/3801738

Daftar Isi:

Magnetic susceptibility was measured on section halves on the Section Half Multisensor Logger (SHMSL) using a Bartington MS2 meter and either a MS2E or MS2K probe. Because all JRSO cores meet minimum size requirements for these two probes, MSPOINT data are corrected for volume and recorded in SI susceptibility units (x10-5).