Low-degree melt metasomatic origin of heavy Fe isotope enrichment in the MORB mantle
(2022)
Journal Article
Studies of mid-ocean ridge basalts (MORB) show a variable Fe isotope composition of the oceanic upper mantle. To test a recent hypothesis that heavy Fe isotope enrichment in the MORB mantle results from the same process of incompatible element enrich... Read More about Low-degree melt metasomatic origin of heavy Fe isotope enrichment in the MORB mantle.