Physical properties of sediment cores TG-01, Ona Basin, southwestern Scotia Sea (Antarctica) ...

During expedition SCAN 2013, gravity core TG-01 was collected in the Ona High slope, central Ona Basin, NE prolongation of the Antarctic Peninsula. The core is 400 cm long and was collected from 2160 m water depth at 60º22'23.9314''S, 53º02'15.2501''W. Non-destructive a...

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Bibliographic Details
Main Authors: López-Quirós, Adrián, Lobo, Francisco J, Duffy, Meghan, Leventer, Amy, Evangelinos, Dimitris, Escutia, Carlota, Bohoyo, Fernando
Format: Dataset
Language:English
Published: PANGAEA 2021
Subjects:
Antarctica
Deglaciation
Diatom assemblage
Late Quaternary
LGM
Scotia Sea
Seismic stratigraphy
DEPTH, sediment/rock
Core section number
Sample thickness
Velocity, compressional wave
Density, wet bulk
Magnetic susceptibility, mass
Magnetic susceptibility
Resistivity, electrical
Gravity corer
Multi-Sensor Core Logger MSCL, GEOTEK
SCAN2013
Hespérides
Antarctic
The Antarctic
Antarctic Peninsula
Ona Basin
Antarc*
Online Access:https://dx.doi.org/10.1594/pangaea.931796
https://doi.pangaea.de/10.1594/PANGAEA.931796
Description
Summary:During expedition SCAN 2013, gravity core TG-01 was collected in the Ona High slope, central Ona Basin, NE prolongation of the Antarctic Peninsula. The core is 400 cm long and was collected from 2160 m water depth at 60º22'23.9314''S, 53º02'15.2501''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). ...

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