Redox freezing and melting in the Earth's deep mantle resulting from carbon-iron redox coupling.
about
Synthesis of heavy hydrocarbons at the core-mantle boundary.Structural complexity of simple Fe2O3 at high pressures and temperaturesOrigins of ultralow velocity zones through slab-derived metallic meltHigh-pressure orthorhombic ferromagnesite as a potential deep-mantle carbon carrierCarbon-bearing iron phases and the carbon isotope composition of the deep Earth.Carbon-bearing silicate melt at deep mantle conditions.Structures of dolomite at ultrahigh pressure and their influence on the deep carbon cycle.Redox heterogeneity in mid-ocean ridge basalts as a function of mantle source.Disproportionation of (Mg,Fe)SiO₃ perovskite in Earth's deep lower mantle.First direct evidence of sedimentary carbonate recycling in subduction-related xenoliths.Mantle-slab interaction and redox mechanism of diamond formation.Stability of iron-bearing carbonates in the deep Earth's interior.Slab melting as a barrier to deep carbon subduction.Diamond formation in the deep lower mantle: a high-pressure reaction of MgCO3 and SiO2.Carbon and Nitrogen Speciation in N-poor C-O-H-N Fluids at 6.3 GPa and 1100-1400 °C.Redox-freezing and nucleation of diamond via magnetite formation in the Earth's mantle.Carbon-dioxide-rich silicate melt in the Earth's upper mantle.The oxidation state of the mantle and the extraction of carbon from Earth's interior.Implications for metal and volatile cycles from the pH of subduction zone fluids.Transport properties of carbonated silicate melt at high pressure.Natural diamond formation by self-redox of ferromagnesian carbonate.Large gem diamonds from metallic liquid in Earth's deep mantle.Deep mantle cycling of oceanic crust: evidence from diamonds and their mineral inclusions.Active carbon sequestration in the Alpine mantle wedge and implications for long-term climate trends.Crystalline polymeric carbon dioxide stable at megabar pressuresExperimental investigation of the stability of Fe-rich carbonates in the lower mantleThe stability of magnesite in the transition zone and the lower mantle as function of oxygen fugacityOrigin of sub-lithospheric diamonds from the Juina-5 kimberlite (Brazil): constraints from carbon isotopes and inclusion compositions
P2860
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P2860
Redox freezing and melting in the Earth's deep mantle resulting from carbon-iron redox coupling.
description
2011 nî lūn-bûn
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2011年の論文
@ja
2011年学术文章
@wuu
2011年学术文章
@zh
2011年学术文章
@zh-cn
2011年学术文章
@zh-hans
2011年学术文章
@zh-my
2011年学术文章
@zh-sg
2011年學術文章
@yue
2011年學術文章
@zh-hant
name
Redox freezing and melting in ...... om carbon-iron redox coupling.
@en
Redox freezing and melting in ...... om carbon-iron redox coupling.
@nl
type
label
Redox freezing and melting in ...... om carbon-iron redox coupling.
@en
Redox freezing and melting in ...... om carbon-iron redox coupling.
@nl
prefLabel
Redox freezing and melting in ...... om carbon-iron redox coupling.
@en
Redox freezing and melting in ...... om carbon-iron redox coupling.
@nl
P2860
P356
P1433
P1476
Redox freezing and melting in ...... om carbon-iron redox coupling.
@en
P2093
Arno Rohrbach
Max W Schmidt
P2860
P2888
P304
P356
10.1038/NATURE09899
P407
P577
2011-03-23T00:00:00Z
P5875
P6179
1021907929