Fe isotope fractionation caused by phase transition of FeS and implications for Fe isotope signatures of the mantle and core
Author:
Publisher
Elsevier BV
Subject
Geochemistry and Petrology
Reference99 articles.
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3. Magnetically driven phonon instability enables the metal-insulator transition in h-FeS;Bansal;Nat. Phys.,2020
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5. Iron isotope fractionation between pyrite (FeS2), hematite (Fe2O3) and siderite (FeCO3): a first-principles density functional theory study;Blanchard;Geochim. Cosmochim. Acta,2009
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