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

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. Th...

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Bibliographic Details
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
okhotsk sea
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.932393
https://doi.org/10.1594/PANGAEA.932393
Description
Summary: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.

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