Magnetic susceptibility and Anhysteretic remanent magnetization in marine sediment core MD01-2414 from the central

• Main Authors: Chou, Yu-Min, Jiang, Xiaodong, Lo, Li, Wang, Liang-Chi, Lee, Teh-Quei, Wang, Chun-Chieh, Pan, Yongxin, Zou, Jiangjun, Humbert, Fabien, Liu, Zhiqiang
• Format: Dataset
• Language: English
• Published: PANGAEA 2021
• Subjects: AGE; Anhysteretic remanent magnetization; Anhysteretic remanent magnetization/magnetic susceptibility ratio; Bartington MS2C sensor; Declination; DEPTH; sediment/rock; environmental magnetism; Giant piston corer; GPC; IMAGES VII - WEPAMA; Inclination; Magnetic susceptibility; marine sediments; Marion Dufresne (1995); MD012414; MD01-2414; MD122; Mid-Brunhes Transition; mid-Pleistocene transition; Okhotsk Sea; paleomagnetism; Relative paleointensity proxy; Sea ice; Sea of Ochotsk; Super-interglacial; terrigenous detritus; okhotsk sea
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.932393; https://doi.org/10.1594/PANGAEA.932393

Magnetic measurements of U-channel samples were measured by the Bartington MS2 magnetic susceptibility system with an ASC auto-tracking rail and a cryogenic magnetometer (2G 755 SRM) in the shielding room of the paleomagnetic laboratory at the Institute of Earth Sciences, Academia Sinica, Taiwan. The Anhysteretic Remanent Magnetization (ARM) was applied with a DC bias field of 1 Gauss under a 100 mT alternating field. All U-channel measurements are within 1 cm interval.