Iron K-edge X-ray absorption spectroscopy of dust particles from the Talos Dome ice core (East Antarctica) and Jarosite abundance

General information (depth along the core, age, extracted dust) of the samples analyzed through synchrtorn radiation at B18 beamline (Diamond Light Source Synchrotron), including Fe K-edge energy position and jarosite relative contribution. The AICC2012 chronolgy have been used (Veres et al. 2013, B...

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Bibliographic Details
Main Authors: Baccolo, Giovanni, Delmonte, Barbara, Niles, Paul B, Cibin, Giannantonio, Di Stefano, Elena, Hampai, Dariush, Keller, Lindsay, Maggi, Valter, Marcelli, Augusto, Michalski, Joseph, Snead, Cristopher, Frezzotti, Massimo
Format: Dataset
Language:English
Published: PANGAEA 2020
Subjects:
AGE
Antarctica
DEPTH
ice/snow
ice cores
ICEDRILL
Ice drill
Iron Geochemistry
Iron K-edge energy
Iron K-edge energy error
Jarosite
error
Mineral dust
mineralogy
Period (Geological Time Scale)
Sample ID
Sample mass
TALDICE
Talos_Dome
Talos Dome Ice Core
East Antarctica
Talos Dome
Antarc*
ice core
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.924113
https://doi.org/10.1594/PANGAEA.924113
Description
Summary:General information (depth along the core, age, extracted dust) of the samples analyzed through synchrtorn radiation at B18 beamline (Diamond Light Source Synchrotron), including Fe K-edge energy position and jarosite relative contribution. The AICC2012 chronolgy have been used (Veres et al. 2013, Bazin et al. 2013).

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