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...
Published in: | Contributions to Mineralogy and Petrology |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Springer
2022
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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 |