Magnetic susceptibility and Anhysteretic remanent magnetization in marine sediment core MD01-2414 from the central
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| Main Authors: | , , , , , , , , , |
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| Format: | Dataset Open Access |
| Language: | en |
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PANGAEA
2021
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| _version_ | 1867172167866646528 |
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| 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 |