Europium in plagioclase-hosted melt inclusions reveals mantle melting modulates oxygen fugacity

Abstract To gain insights into the composition and heterogeneity of Earth’s interior, the partial pressure of oxygen (oxygen fugacity, or fO2) in igneous rocks is characterized. A surprising observation is that relative to reference buffers, fO2s of mantle melts (mid-ocean ridge basalts, or MORBs) a...

詳細記述

書誌詳細
主要な著者: Nicholas Dygert, Gokce K. Ustunisik, Roger L. Nielsen
フォーマット: 論文
言語:English
出版事項: Nature Portfolio 2024-04-01
シリーズ:Nature Communications
オンライン・アクセス:https://doi.org/10.1038/s41467-024-47224-5