IODP Expedition 392 Magnetic remanence (SRM-longcore)

• Main Authors: Uenzelmann-Neben, Gabriele, Bohaty, Steven M., Childress, Laurel B., Archontikis, Odysseas A., Batenburg, Sietske J., Bijl, Peter K., Burkett, Ashley M., Cawthra, Hayley C., Chanda, Pratyusha, Coenen, Jason J., Dallanave, Edoardo, Davidson, Peter C., Doiron, Kelsey E., Geldmacher, Jörg, Gürer, Derya, Haynes, Shannon J., Herrle, Jens O., Ichiyama, Yuji, Jana, Debadrita, Jones, Matthew M., Kato, Chie, Kulhanek, Denise K., Li, Juan, Liu, Jia, McManus, James, Minakov, Alexander N., Penman, Donald E., Sprain, Courtney J., Tessin, Allyson C., Wagner, Thomas, Westerhold, Thomas
• Other Authors: International Ocean Discovery Program
• Format: Other/Unknown Material
• Language: unknown
• Published: Zenodo 2023
• Subjects: International Ocean Discovery Program; IODP; JOIDES Resolution; Expedition 392; Site U1579; Site U1580; Site U1581; Site U1582; Algulhas Plateau Cretaceous Climate; Earth connections; Climate and ocean change; K/Pg boundary; large igneous province; PETM; LIP; zeolite authigenesis; Paleocene-Eocene Thermal Maximum; igneous sill intrusion; Campanian; Oligocene pelagic carbonates; paleoceanography; African-Southern Ocean Gateway; Southern Ocean
• Online Access: https://doi.org/10.5281/zenodo.8277840

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.