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, Bazin et al. 2013).

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