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Main Authors: López-Quirós, Adrián, Lobo, Francisco J, Duffy, Meghan, Leventer, Amy, Evangelinos, Dimitris, Escutia, Carlota, Bohoyo, Fernando
Format: Dataset Open Access
Language:en
Published: PANGAEA 2021
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Online Access:https://doi.org/10.1594/PANGAEA.931838
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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, two gravity cores were collected in the Ona High slope, central Ona Basin, NE prolongation of the Antarctic Peninsula. Core TG-01 is 400 cm long and was collected from 2160 m water depth at 60º22'23.9314''S, 53º02'15.2501''W; core TG-03 is 295 cm long and was obtained from 2789 m water depth at 60º11'23.4003''S, 53º10'49.0810''W. Non-destructive analyses (i.e., physical properties measurements and X-ray fluorescence scanning) were performed on the archive halves. Both, physical properties (magnetic susceptibility, gamma-ray density, electrical resistivity and P-wave velocity) and major element compositions 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_931838
institution PANGAEA
language en
publishDate 2021
publisher PANGAEA
record_format pangaea
spellingShingle Physical properties and XRF scanner data of sediment cores TG-01 and 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; Deglaciation; Diatom assemblage; Late Quaternary; LGM; Scotia Sea; Seismic stratigraphy
During expedition SCAN 2013, two gravity cores were collected in the Ona High slope, central Ona Basin, NE prolongation of the Antarctic Peninsula. Core TG-01 is 400 cm long and was collected from 2160 m water depth at 60º22'23.9314''S, 53º02'15.2501''W; core TG-03 is 295 cm long and was obtained from 2789 m water depth at 60º11'23.4003''S, 53º10'49.0810''W. Non-destructive analyses (i.e., physical properties measurements and X-ray fluorescence scanning) were performed on the archive halves. Both, physical properties (magnetic susceptibility, gamma-ray density, electrical resistivity and P-wave velocity) and major element compositions 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 and XRF scanner data of sediment cores TG-01 and TG-03, Ona Basin, southwestern Scotia Sea (Antarctica)
topic Antarctica; Deglaciation; Diatom assemblage; Late Quaternary; LGM; Scotia Sea; Seismic stratigraphy
url https://doi.org/10.1594/PANGAEA.931838