Testing the Homogeneity of the Solar System for Iron (54, 56, 57, and 58) and Tungsten (182, 183, 184, and 186) Isotope Abundances

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Scientific paper

The solar nebula was homogenized at a planetary scale at the 0.2 epsilon
and 0.5 epsilon level for iron-56 and iron-58, respectively. Preliminary
results seem to indicate the presence of a s-process tungsten component
in leaching experiments of primitive meteorites.

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