Читать книгу Magma Redox Geochemistry - Группа авторов - Страница 24

The redox state and its evolution in Earth’s interior are established as a result of (i) early accretion under the influence of variably oxidized building blocks and late‐stage meteoritic impact; (ii) magma ocean(s) formation, core segregation, and mantle crystallization; (iii) establishment of mantle convection exhuming early‐generated deep heterogeneities; and (iv) recycling of surface materials by (initially regional and episodic) subduction processes.