Iron, zinc, magnesium and uranium isotopic fractionation during continental crust differentiation: The tale from migmatites, granitoids, and pegmatites

Volume: 97, Pages: 247 - 265
Published: Nov 15, 2012
Abstract
null null The causes of some stable isotopic variations in felsic rocks are not well understood. In particular, the origin of the heavy Fe isotopic compositions ( i.e. , high δ 56 Fe values, deviation in ‰ of the null 56 Fe/ 54 Fe ratio relative to IRMM-014) of granites with SiO 2  > 70 wt.% compared with less silicic rocks is still debated. It has been interpreted to reflect isotopic fractionation during late stage aqueous fluid exsolution,...
Paper Details
Title
Iron, zinc, magnesium and uranium isotopic fractionation during continental crust differentiation: The tale from migmatites, granitoids, and pegmatites
Published Date
Nov 15, 2012
Volume
97
Pages
247 - 265
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