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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.931797 |
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| _version_ | 1867168499109986304 |
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| author | López-Quirós, Adrián Lobo, Francisco J Duffy, Meghan Leventer, Amy Evangelinos, Dimitris Escutia, Carlota Bohoyo, Fernando |
| author_facet | López-Quirós, Adrián Lobo, Francisco J Duffy, Meghan Leventer, Amy Evangelinos, Dimitris Escutia, Carlota Bohoyo, Fernando |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | During expedition SCAN 2013, gravity core TG-03 was collected in the Ona High slope, central Ona Basin, NE prolongation of the Antarctic Peninsula. The core is 295 cm long and was collected from 2789 m water depth at 60º11'23.4003''S, 53º10'49.0810''W. Non-destructive analyses were performed on the archive halves. Physical properties (magnetic susceptibility, gamma-ray density, electrical resistivity and P-wave velocity) were determined at 1-cm resolution on split core surfaces of the archive halves using a GEOTEK Multi-Sensor Core Logger (MSCL) 81 at the Spanish Geological Survey (IGME, Spain). |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_931797 |
| institution | PANGAEA |
| language | en |
| publishDate | 2021 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Physical properties of sediment cores TG-03, Ona Basin, southwestern Scotia Sea (Antarctica) López-Quirós, Adrián Lobo, Francisco J Duffy, Meghan Leventer, Amy Evangelinos, Dimitris Escutia, Carlota Bohoyo, Fernando Antarctica; Core section number; Deglaciation; Density, wet bulk; DEPTH, sediment/rock; Diatom assemblage; GC; Gravity corer; Hespérides; Late Quaternary; LGM; Magnetic susceptibility; Magnetic susceptibility, mass; Multi-Sensor Core Logger (MSCL), GEOTEK; Resistivity, electrical; Sample thickness; SCAN2013; SCAN 2013; Scotia Sea; Seismic stratigraphy; TG-03; Velocity, compressional wave During expedition SCAN 2013, gravity core TG-03 was collected in the Ona High slope, central Ona Basin, NE prolongation of the Antarctic Peninsula. The core is 295 cm long and was collected from 2789 m water depth at 60º11'23.4003''S, 53º10'49.0810''W. Non-destructive analyses were performed on the archive halves. Physical properties (magnetic susceptibility, gamma-ray density, electrical resistivity and P-wave velocity) were determined at 1-cm resolution on split core surfaces of the archive halves using a GEOTEK Multi-Sensor Core Logger (MSCL) 81 at the Spanish Geological Survey (IGME, Spain). |
| title | Physical properties of sediment cores TG-03, Ona Basin, southwestern Scotia Sea (Antarctica) |
| topic | Antarctica; Core section number; Deglaciation; Density, wet bulk; DEPTH, sediment/rock; Diatom assemblage; GC; Gravity corer; Hespérides; Late Quaternary; LGM; Magnetic susceptibility; Magnetic susceptibility, mass; Multi-Sensor Core Logger (MSCL), GEOTEK; Resistivity, electrical; Sample thickness; SCAN2013; SCAN 2013; Scotia Sea; Seismic stratigraphy; TG-03; Velocity, compressional wave |
| url | https://doi.org/10.1594/PANGAEA.931797 |