Melting Behavior of B1 FeO Up To 186 GPa: Existence of FeO‐Rich Melts in the Lowermost Mantle
FeO is an important component in both mantle silicates and core iron alloys. Understanding its melting behavior and physical properties is crucial for exploring the chemistry and physics of our planet.
Suyu Fu, Kei Hirose
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Insights on Upper Mantle Melting, Rheology, and Anelastic Behavior From Seismic Shear Wave Tomography. [PDF]
Cobden L, Trampert J, Fichtner A.
europepmc +1 more source
Mantle melting and lithospheric structure beneath eastern Australia's Cenozoic volcanoes from 3D magnetotellurics. [PDF]
Margiono R, Heinson G.
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Onset of slab mantle melting in Earth's lower mantle: Evidence from ferropericlase in superdeep diamonds. [PDF]
Ni P +15 more
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Magnetotelluric evidence for highly focused mantle melting along the ultraslow-spreading Gakkel Ridge, Arctic Ocean. [PDF]
Zhang T +16 more
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Correlated crustal and mantle melting documents proto-Tibetan Plateau growth. [PDF]
Li W +6 more
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Generation of carbonated peridotite melts via biogenic sediment recycling in modern subduction zones. [PDF]
Errázuriz-Henao C +9 more
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Continental evolution influenced by relamination of deeply subducted continental crust. [PDF]
Gómez-Frutos D +3 more
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Collapse and resurgence of the Iceland mantle plume. [PDF]
Pearman C +8 more
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Progressive sub-arc mantle oxidation modulated by sediment melt. [PDF]
Gao M, Wang Y, Xu YG.
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