Original paper
Origin of heavy Fe isotope compositions in high-silica igneous rocks: A rhyolite perspective
Abstract
The origin of heavy Fe isotope compositions in high-silica (>70 wt% SiO2) igneous rocks remains a highly controversial topic. Considering that fluid exsolution in eruptive rocks is more straight-forward to constrain than in plutonic rocks, this study addresses the problem of Fe isotope fractionation in high-silica igneous rocks by measuring Fe isotope compositions of representative rhyolitic samples from the Neoproterozoic volcanic-sedimentary...
Paper Details
Title
Origin of heavy Fe isotope compositions in high-silica igneous rocks: A rhyolite perspective
Published Date
Dec 1, 2017
Volume
218
Pages
58 - 72
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