Rock and paleomagneitc measurements of PS67/197-1
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| Format: | Dataset Open Access |
| Langue: | en |
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PANGAEA
2025
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| _version_ | 1867170134146154496 |
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| author | Xiao, Wenshen Frederichs, Thomas Gersonde, Rainer Esper, Oliver Zhang, Xu |
| author_facet | Xiao, Wenshen Frederichs, Thomas Gersonde, Rainer Esper, Oliver Zhang, Xu |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | The core was taken in 2005 during Polarstern cruise ANT-XXII/4 in the central Scotia Sea. Magnetic susceptibility, further paleomagnetic information and other proxies were measured on this and other cores in order to establish a detailed sediment stratigraphy of the Scotia Sea for the past 300 ka. A description of the methods is given in Xiao et al. (2016). |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_980093 |
| institution | PANGAEA |
| language | en |
| publishDate | 2025 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Rock and paleomagneitc measurements of PS67/197-1 Xiao, Wenshen Frederichs, Thomas Gersonde, Rainer Esper, Oliver Zhang, Xu ANT-XXII/4; Cryogenic magnetometer, 2G Enterprises, 755HR; DEPTH, sediment/rock; Holocene climate variability at high-southern latitudes: an integrated perspective; HOLOCLIP; Inclination; Kappabridge, Geofyzika Brno, KLY-2; Magnetic susceptibility; Magnetic susceptibility, volume; Marine sediment; Natural remanent magnetization; Natural remanent magnetization (NRM); NRM, median destructive field of natural remanent magnetization, alternating field; Paleomagnetics; PC; Piston corer; Polarstern; PS67; PS67/197-1; Relative paleointensity (RPI); Relative paleointensity proxy; Scotia Sea; Slope NRM/ARM (25 - 50 mT); Slope NRM/ARM (25 - 50 mT), standardized; Slope NRM/ARM (25 - 50 mT), standardized and grain size corrected; Slope NRM/IRM (25 , 50 mT), standardized and grain size corrected; Slope NRM/IRM (25 - 50 mT); Slope NRM/IRM (25 - 50 mT), standardized; Southern Ocean The core was taken in 2005 during Polarstern cruise ANT-XXII/4 in the central Scotia Sea. Magnetic susceptibility, further paleomagnetic information and other proxies were measured on this and other cores in order to establish a detailed sediment stratigraphy of the Scotia Sea for the past 300 ka. A description of the methods is given in Xiao et al. (2016). |
| title | Rock and paleomagneitc measurements of PS67/197-1 |
| topic | ANT-XXII/4; Cryogenic magnetometer, 2G Enterprises, 755HR; DEPTH, sediment/rock; Holocene climate variability at high-southern latitudes: an integrated perspective; HOLOCLIP; Inclination; Kappabridge, Geofyzika Brno, KLY-2; Magnetic susceptibility; Magnetic susceptibility, volume; Marine sediment; Natural remanent magnetization; Natural remanent magnetization (NRM); NRM, median destructive field of natural remanent magnetization, alternating field; Paleomagnetics; PC; Piston corer; Polarstern; PS67; PS67/197-1; Relative paleointensity (RPI); Relative paleointensity proxy; Scotia Sea; Slope NRM/ARM (25 - 50 mT); Slope NRM/ARM (25 - 50 mT), standardized; Slope NRM/ARM (25 - 50 mT), standardized and grain size corrected; Slope NRM/IRM (25 , 50 mT), standardized and grain size corrected; Slope NRM/IRM (25 - 50 mT); Slope NRM/IRM (25 - 50 mT), standardized; Southern Ocean |
| url | https://doi.org/10.1594/PANGAEA.980093 |