Fe3+ Distribution and Fe3+/ΣFe-Oxygen Fugacity Variations in Kimberlite-Borne Eclogite Xenoliths, with Comments on Clinopyroxene-Garnet Oxy-Thermobarometry
The valence state of iron in mantle-derived melts, such as mid-ocean ridge basalt, is a useful
proxy for oxygen fugacity (ƒ O2). On subduction, oceanic crust undergoes metamorphic …
proxy for oxygen fugacity (ƒ O2). On subduction, oceanic crust undergoes metamorphic …
Multi-stage ultrahigh temperature metamorphism in the lower crust of the Kaapvaal craton recorded by U–Pb ages of garnet
U–Pb ages were determined by split-stream LA-SF/MC-ICPMS in garnets from UHT
granulite xenoliths (Star mine, South Africa; 124 Ma). They give a considerable age range of …
granulite xenoliths (Star mine, South Africa; 124 Ma). They give a considerable age range of …
A fast open data reduction workflow for the electron microprobe flank method to determine Fe3+/ΣFe contents in minerals
DC Hezel, HE Höfer, A Fichtner - American Mineralogist, 2024 - pubs.geoscienceworld.org
Abstract Knowing the Fe3+/ΣFe ratio in minerals is important to understand the formation
and evolution of minerals and their host rocks. Variable Fe3+/ΣFe in, eg, garnet is …
and evolution of minerals and their host rocks. Variable Fe3+/ΣFe in, eg, garnet is …
A fast open data reduction workflow for the electron microprobe flank method to determine Fe3+/ΣFe contents in minerals
DC Hezel, HE Höfer, A Fichtner - American Mineralogist, 2024 - degruyter.com
Abstract Knowing the Fe3+/ΣFe ratio in minerals is important to understand the formation
and evolution of minerals and their host rocks. Variable Fe3+/ΣFe in, eg, garnet is …
and evolution of minerals and their host rocks. Variable Fe3+/ΣFe in, eg, garnet is …