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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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| Online Access: | https://doi.org/10.1594/PANGAEA.932398 |
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| _version_ | 1867168499315507200 |
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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 | The abundance of iron and manganese were detected by using non-destructive X-ray Fluorescence (XRF) scanning technique. Continuous downcore measurements of element variations were performed in the ITRAX XRF Core Scanner Laboratory, Department of Geosciences, National Taiwan University. All U-channels were scanned by using the 3 kW Mo source and were analyzed at 30 kV/24 mA, 2 mm resolution with a exposure time of 30 s. The count value of each element was calculated from element peak areas of original XRF spectra by the Q-Spec software provided by COX Analytical Systems. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_932398 |
| institution | PANGAEA |
| language | en |
| publishDate | 2021 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Manganese, titanium and iron counts in marine sediment core MD01-2414 from the central Okhotsk Sea 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; DEPTH, sediment/rock; environmental magnetism; Giant piston corer; GPC; IMAGES VII - WEPAMA; Iron; Iron/Titanium ratio; log-Iron/Titanium ratio; log-Manganese/Titanium ratio; Manganese; Manganese/Titanium ratio; marine sediments; Marion Dufresne (1995); MD012414; MD01-2414; MD122; Mid-Brunhes Transition; mid-Pleistocene transition; Okhotsk Sea; paleomagnetism; Sea ice; Sea of Ochotsk; Super-interglacial; Terrigenous detritus; Titanium; X-ray fluorescence (XRF) The abundance of iron and manganese were detected by using non-destructive X-ray Fluorescence (XRF) scanning technique. Continuous downcore measurements of element variations were performed in the ITRAX XRF Core Scanner Laboratory, Department of Geosciences, National Taiwan University. All U-channels were scanned by using the 3 kW Mo source and were analyzed at 30 kV/24 mA, 2 mm resolution with a exposure time of 30 s. The count value of each element was calculated from element peak areas of original XRF spectra by the Q-Spec software provided by COX Analytical Systems. |
| title | Manganese, titanium and iron counts in marine sediment core MD01-2414 from the central Okhotsk Sea |
| topic | AGE; DEPTH, sediment/rock; environmental magnetism; Giant piston corer; GPC; IMAGES VII - WEPAMA; Iron; Iron/Titanium ratio; log-Iron/Titanium ratio; log-Manganese/Titanium ratio; Manganese; Manganese/Titanium ratio; marine sediments; Marion Dufresne (1995); MD012414; MD01-2414; MD122; Mid-Brunhes Transition; mid-Pleistocene transition; Okhotsk Sea; paleomagnetism; Sea ice; Sea of Ochotsk; Super-interglacial; Terrigenous detritus; Titanium; X-ray fluorescence (XRF) |
| url | https://doi.org/10.1594/PANGAEA.932398 |