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Stability of Fe,Al-bearing bridgmanite in the lower mantle and synthesis of pure Fe-bridgmanite.Terapascal static pressure generation with ultrahigh yield strength nanodiamondPhase transition induced strain in ZnO under high pressureMultiple seismic reflectors in Earth's lowermost mantle.High-pressure orthorhombic ferromagnesite as a potential deep-mantle carbon carrierThermodynamics and Equations of State of Iron to 350 GPa and 6000 K.Stress-induced nanoparticle crystallizationX-ray diffraction in the pulsed laser heated diamond anvil cell.Seismic anisotropy of the D″ layer induced by (001) deformation of post-perovskiteImplementation of micro-ball nanodiamond anvils for high-pressure studies above 6 Mbar.Portable double-sided laser-heating system for Mössbauer spectroscopy and X-ray diffraction experiments at synchrotron facilities with diamond anvil cells.BX90: a new diamond anvil cell design for X-ray diffraction and optical measurements.Combined resistive and laser heating technique for in situ radial X-ray diffraction in the diamond anvil cell at high pressure and temperature.New host for carbon in the deep Earth.Simulation of the planetary interior differentiation processes in the laboratoryDisproportionation of (Mg,Fe)SiO₃ perovskite in Earth's deep lower mantle.Discovery of the recoverable high-pressure iron oxide Fe4O5.Stable magnesium peroxide at high pressure.Single-crystal structure determination of (Mg,Fe)SiO3 postperovskiteIcosahedral AlCuFe quasicrystal at high pressure and temperature and its implications for the stability of icosahedrite.The equation of state of the Pmmn phase of NiSi.Stability of iron-bearing carbonates in the deep Earth's interior.Dehydrogenation of goethite in Earth's deep lower mantle.Diamond formation in the deep lower mantle: a high-pressure reaction of MgCO3 and SiO2.Compressional pathways of α-cristobalite, structure of cristobalite X-I, and towards the understanding of seifertite formationThe phase diagram of ammonium nitrate.High-temperature experiments using a resistively heated high-pressure membrane diamond anvil cell.FeO2 and FeOOH under deep lower-mantle conditions and Earth's oxygen-hydrogen cycles.Hydrogen-bearing iron peroxide and the origin of ultralow-velocity zones.Beyond sixfold coordinated Si in SiO2 glass at ultrahigh pressures.Compression Freezing Kinetics of Water to Ice VII.The most incompressible metal osmium at static pressures above 750 gigapascals.Experimental evidence of superionic conduction in H2O ice.Nature of the Volume Isotope Effect in Ice.Fundamental high-pressure calibration from all-electron quantum Monte Carlo calculations.Discovery of a hexagonal ultradense hydrous phase in (Fe,Al)OOHThermal expansion of SiC at high pressure-temperature and implications for thermal convection in the deep interiors of carbide exoplanetsExperimental method for in situ determination of material textures at simultaneous high pressure and high temperature by means of radial diffraction in the diamond anvil cellHigh-pressure behavior and P -induced phase transition of CaB3 O4 (OH)3 ·H2 O (colemanite)Pargasite at high pressure and temperature
P2860
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P2860
description
2007 nî lūn-bûn
@nan
2007 թուականի Մայիսին հրատարակուած գիտական յօդուած
@hyw
2007 թվականի մայիսին հրատարակված գիտական հոդված
@hy
2007年の論文
@ja
2007年論文
@yue
2007年論文
@zh-hant
2007年論文
@zh-hk
2007年論文
@zh-mo
2007年論文
@zh-tw
2007年论文
@wuu
name
Toward an internally consistent pressure scale
@ast
Toward an internally consistent pressure scale
@en
type
label
Toward an internally consistent pressure scale
@ast
Toward an internally consistent pressure scale
@en
prefLabel
Toward an internally consistent pressure scale
@ast
Toward an internally consistent pressure scale
@en
P2093
P2860
P356
P1476
Toward an internally consistent pressure scale
@en
P2093
Angele Ricolleau
Kenji Mibe
Mark Frank
Vitali Prakapenka
Yingwei Fei
P2860
P304
P356
10.1073/PNAS.0609013104
P407
P50
P577
2007-05-02T00:00:00Z