XRF scanner data 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 - Data Publisher for Earth & Environmental Science 2021
Subjects:
Antarctica
Deglaciation
Diatom assemblage
Late Quaternary
LGM
Scotia Sea
Seismic stratigraphy
DEPTH, sediment/rock
Magnesium
Aluminium
Silicon
Phosphorus
Sulfur
Chlorine
Potassium
Calcium
Scandium
Titanium
Vanadium
Chromium
Manganese
Iron
Cobalt
Nickel
Copper
Zinc
Gallium
Arsenic
Bromine
Rubidium
Strontium
Yttrium
Zirconium
Gravity corer
X-ray fluorescence XRF
SCAN2013
Hespérides
Antarctic
Antarctic Peninsula
Ona Basin
The Antarctic
Antarc*
Online Access:https://dx.doi.org/10.1594/pangaea.931798
https://doi.pangaea.de/10.1594/PANGAEA.931798
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 (i.e., X-ray fluorescence scanning) were performed on the archive halves. 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).

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