about
Synthesis of heavy hydrocarbons at the core-mantle boundary.Reevaluating carbon fluxes in subduction zones, what goes down, mostly comes upPlate tectonic controls on atmospheric CO2 levels since the TriassicOrigins of ultralow velocity zones through slab-derived metallic meltHidden carbon in Earth's inner core revealed by shear softening in dense Fe7C3High-pressure orthorhombic ferromagnesite as a potential deep-mantle carbon carrierCarbon-bearing iron phases and the carbon isotope composition of the deep Earth.Redox preconditioning deep cratonic lithosphere for kimberlite genesis - evidence from the central Slave Craton.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.First direct evidence of sedimentary carbonate recycling in subduction-related xenoliths.Tracing the ingredients for a habitable earth from interstellar space through planet formation.Degassing of reduced carbon from planetary basaltsMantle-slab interaction and redox mechanism of diamond formation.Petit-spot as definitive evidence for partial melting in the asthenosphere caused by CO2Remobilization of crustal carbon may dominate volcanic arc emissions.Sea level fall during glaciation stabilized atmospheric CO2 by enhanced volcanic degassing.Molecular dynamics simulations of a lithium/sodium carbonate mixture.The lower pT limit of deep hydrocarbon synthesis by CaCO3 aqueous reduction.Slab melting as a barrier to deep carbon subduction.Linking mantle plumes, large igneous provinces and environmental catastrophes.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.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.Redox freezing and melting in the Earth's deep mantle resulting from carbon-iron redox coupling.Water and hydrogen are immiscible in Earth's mantle.Implications for metal and volatile cycles from the pH of subduction zone fluids.Pressure driven spin transition in siderite and magnesiosiderite single crystals.Multi-scale magnetic mapping of serpentinite carbonation.Transport properties of carbonated silicate melt at high pressure.Large gem diamonds from metallic liquid in Earth's deep mantle.Experimental investigation of the stability of Fe-rich carbonates in the lower mantleTwo-step rise of atmospheric oxygen linked to the growth of continentsThe habitability of a stagnant-lid EarthAbundant carbon in the mantle beneath Hawai‘iHigh-pressure polymorphism and structural transitions of norsethite, BaMg(CO3)2The origin of volatiles in the Earth's mantlePotential links between continental rifting, CO2 degassing and climate change through time
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P2860
description
im September 2010 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована у вересні 2010
@uk
name
The deep carbon cycle and melting in Earth's interior
@en
The deep carbon cycle and melting in Earth's interior
@nl
type
label
The deep carbon cycle and melting in Earth's interior
@en
The deep carbon cycle and melting in Earth's interior
@nl
prefLabel
The deep carbon cycle and melting in Earth's interior
@en
The deep carbon cycle and melting in Earth's interior
@nl
P1476
The deep carbon cycle and melting in Earth's interior
@en
P2093
Marc M. Hirschmann
P356
10.1016/J.EPSL.2010.06.039
P407
P577
2010-09-15T00:00:00Z