The mantle source of basalts from Reunion Island is not more oxidized than the MORB source mantle

Glasses quenched from relatively undegassed ocean island magmas erupted from volcanoes at Iceland, Hawaii, the Canary Islands, and Erebus have elevated Fe³⁺/∑Fe ratios compared to glasses quenched from mid-ocean ridge basalts. This has been ascribed to elevated fO₂ of their mantle sources, plausibly...

Full description

Bibliographic Details
Published in:Contributions to Mineralogy and Petrology
Main Authors: Brounce, Maryjo, Stolper, Edward, Eiler, John
Format: Article in Journal/Newspaper
Language:English
Published: Springer 2022
Subjects:
Online Access:https://authors.library.caltech.edu/112503/
https://authors.library.caltech.edu/112503/1/2021_Article_.pdf
https://authors.library.caltech.edu/112503/2/410_2021_1870_MOESM1_ESM.docx
https://resolver.caltech.edu/CaltechAUTHORS:20211217-10741800