about
Toward a mineral physics reference model for the Moon's core.Compressed glassy carbon: An ultrastrong and elastic interpenetrating graphene network.Experimental evidence that potassium is a substantial radioactive heat source in planetary cores.Simulation of the planetary interior differentiation processes in the laboratoryReversible switching between pressure-induced amorphization and thermal-driven recrystallization in VO2(B) nanosheets.Icosahedral AlCuFe quasicrystal at high pressure and temperature and its implications for the stability of icosahedrite.Recovery of an oxidized majorite inclusion from Earth's deep asthenosphere.Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions.Size tunable synthesis of solution processable diamond nanocrystals.Cold deep subduction recorded by remnants of a Paleoproterozoic carbonated slabSecond critical endpoint in the peridotite-H2O systemThe compression behavior of blödite at low and high temperature up to ∼10 GPa: Implications for the stability of hydrous sulfates on icy planetary bodiesA high-pressure synthesis of hydrothermally stable periodic mesoporous crystalline aluminosilica materialsElectrical resistivity of substitutionally disordered hcp Fe–Si and Fe–Ni alloys: Chemically-induced resistivity saturation in the Earth's coreEquation of state of the high-pressure Fe3O4phase and a new structural transition at 70 GPaExperimental constraints on the formation of the Tibetan podiform chromititesPhase stabilities and spin transitions of Fe3(S1−xPx) at high pressure and its implications in meteoritesProbing carbon-bearing species and CO2inclusions in amorphous carbon-MgSiO3enstatite reaction products at 1.5 GPa: Insights from13C high-resolution solid-state NMRThermal equation of state of hcp-iron: Constraint on the density deficit of Earth's solid inner coreThermometry of the magma ocean: Controls on the metal–silicate partitioning of goldRecoil-free fractions of iron in aluminous bridgmanite from temperature-dependent Mössbauer spectraHigh-pressure synthesis of mesoporous stishovite: potential applications in mineral physicsHow Depth is the Tibetan Chromite: Experimental StudyMicroscopic structural change in a liquid Fe-C alloy of ~5 GPaQuasicrystals at extreme conditions: The role of pressure in stabilizing icosahedral Al63Cu24Fe13at high temperatureExperimental study and thermodynamic calculations of phase relations in the Fe–C system at high pressureHigh-pressure behavior of Fe3P and the role of phosphorus in planetary coresThe effect of Fe on the stability of dolomite at high pressure: Experimental study and petrological observation in eclogite from southwestern Tianshan, ChinaEffect of carbon, sulfur and silicon on iron melting at high pressure: Implications for composition and evolution of the planetary terrestrial coresElectrical and thermal transport properties of iron and iron-silicon alloy at high pressureExperimental determination of siderite stability at high pressureHigh pressure and temperature electrical resistivity of iron and implications for planetary coresInvestigation of High-Pressure and Temperature Behavior of Surfactant-Containing Periodic Mesostructured SilicasMelting Earth's CoreShock compression of Fe-FeS mixture up to 204 GPaInternally consistent thermodynamic database for iron to the Earth's core conditionsMelting behavior of (Mg,Fe)O solid solutions at high pressurePrefaceHigh-pressure crystal chemistry of nickel sulphidesSubsolidus and melting phase relations of basaltic composition in the uppermostlower mantle
P50
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P50
description
onderzoeker
@nl
researcher ORCID ID = 0000-0001-9955-5353
@en
name
Yingwei Fei
@ast
Yingwei Fei
@en
Yingwei Fei
@es
Yingwei Fei
@nl
type
label
Yingwei Fei
@ast
Yingwei Fei
@en
Yingwei Fei
@es
Yingwei Fei
@nl
prefLabel
Yingwei Fei
@ast
Yingwei Fei
@en
Yingwei Fei
@es
Yingwei Fei
@nl
P244
P1053
F-3709-2011
P106
P214
17147093660225000913
P244
P31
P3829
P496
0000-0001-9955-5353
P7859
lccn-n00013077