_version_ 1867172167866646528
author Chou, Yu-Min
Jiang, Xiaodong
Lo, Li
Wang, Liang-Chi
Lee, Teh-Quei
Wang, Chun-Chieh
Pan, Yongxin
Zou, Jiangjun
Humbert, Fabien
Liu, Zhiqiang
author_facet Chou, Yu-Min
Jiang, Xiaodong
Lo, Li
Wang, Liang-Chi
Lee, Teh-Quei
Wang, Chun-Chieh
Pan, Yongxin
Zou, Jiangjun
Humbert, Fabien
Liu, Zhiqiang
collection Datos científicos de ciencias marinas y ambientales
contents 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.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_932393
institution PANGAEA
language en
publishDate 2021
publisher PANGAEA
record_format pangaea
spellingShingle Magnetic susceptibility and Anhysteretic remanent magnetization in marine sediment core MD01-2414 from the central
Chou, Yu-Min
Jiang, Xiaodong
Lo, Li
Wang, Liang-Chi
Lee, Teh-Quei
Wang, Chun-Chieh
Pan, Yongxin
Zou, Jiangjun
Humbert, Fabien
Liu, Zhiqiang
AGE; Anhysteretic remanent magnetization; Anhysteretic remanent magnetization/magnetic susceptibility ratio; Declination; DEPTH, sediment/rock; environmental magnetism; Giant piston corer; GPC; IMAGES VII - WEPAMA; Inclination; Magnetic susceptibility; Magnetic susceptibility meter, Bartington MS2C sensor; 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
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.
title Magnetic susceptibility and Anhysteretic remanent magnetization in marine sediment core MD01-2414 from the central
topic AGE; Anhysteretic remanent magnetization; Anhysteretic remanent magnetization/magnetic susceptibility ratio; Declination; DEPTH, sediment/rock; environmental magnetism; Giant piston corer; GPC; IMAGES VII - WEPAMA; Inclination; Magnetic susceptibility; Magnetic susceptibility meter, Bartington MS2C sensor; 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
url https://doi.org/10.1594/PANGAEA.932393