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
Core section number
Deglaciation
Density
wet bulk
DEPTH
sediment/rock
Diatom assemblage
GC
Gravity corer
Hespérides
Late Quaternary
LGM
Magnetic susceptibility
mass
Multi-Sensor Core Logger (MSCL)
GEOTEK
Resistivity
electrical
Sample thickness
SCAN2013
SCAN 2013
Scotia Sea
Seismic stratigraphy
TG-01
Velocity
compressional wave
Antarc*
Antarctic
Antarctic Peninsula
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.931796
https://doi.org/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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