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Partitioning of Si and platinum group elements between liquid and solid Fe–Si alloys

Geochimica et cosmochimica acta, 2014-05, Vol.132, p.94-100

2014

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Composition of the core from gallium metal–silicate partitioning experiments

Earth and planetary science letters, 2015-10, Vol.427 (C), p.191-201

2015

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Electronic Transitions in Perovskite: Possible Nonconvecting Layers in the Lower Mantle

Science (American Association for the Advancement of Science), 2004-07, Vol.305 (5682), p.383-386

2004

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Low Velocity Zones in the Martian Upper Mantle Highlighted by Sound Velocity Measurements

Geophysical research letters, 2021-10, Vol.48 (19), p.n/a

2021

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Iron Partitioning in Earth's Mantle: Toward a Deep Lower Mantle Discontinuity

Science (American Association for the Advancement of Science), 2003-05, Vol.300 (5620), p.789-791

2003

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Investigating Earth's Formation History Through Copper and Sulfur Metal‐Silicate Partitioning During Core‐Mantle Differentiation

Journal of geophysical research. Solid earth, 2018-10, Vol.123 (10), p.8349-8363

2018

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Effect of composition, structure, and spin state on the thermal conductivity of the Earth's lower mantle

Physics of the earth and planetary interiors, 2010-06, Vol.180 (3), p.148-153

2010

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Reply to Comment by Jennings et al. on “Investigating Earth's Formation History Through Copper and Sulfur Metal‐Silicate Partitioning During Core‐Mantle Differentiation”

Journal of geophysical research. Solid earth, 2019-12, Vol.124 (12), p.12845-12853

2019

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Pressure-Induced High-Spin to Low-Spin Transition in FeS Evidenced by X-Ray Emission Spectroscopy

Physical review letters, 1999-04, Vol.82 (16), p.3284-3287

1999

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Sound Velocities in Iron to 110 Gigapascals

Science (American Association for the Advancement of Science), 2001-01, Vol.291 (5503), p.468-471

2001

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Elasticity of cobalt at high pressure studied by inelastic X-ray scattering

Physical review letters, 2004-11, Vol.93 (21), p.215505.1-215505.4, Article 215505

2004

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Electronic properties of transition-metal oxides under high pressure revealed by x-ray emission spectroscopy

Journal of physics. Condensed matter, 2005-03, Vol.17 (11), p.S717-S726

2005

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Silicon isotopes in angrites and volatile loss in planetesimals

Proceedings of the National Academy of Sciences - PNAS, 2014-12, Vol.111 (48), p.17029-17032

2014

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Application of inelastic X-ray scattering to the measurements of acoustic wave velocities in geophysical materials at very high pressure

Physics of the earth and planetary interiors, 2004-06, Vol.143, p.5-18

2004

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Synthesis and characterization of a binary noble metal nitride

Nature materials, 2004-05, Vol.3 (5), p.294-297

2004

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Oxygen as a light element: A solution to single-stage core formation

Earth and planetary science letters, 2009-10, Vol.288 (1), p.108-114

2009

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Low argon solubility in silicate melts at high pressure

Nature (London), 1998-05, Vol.393 (6683), p.352-355

1998

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Experimental evidence for a high-pressure isostructural phase transition in osmium

Physical review letters, 2004-08, Vol.93 (9), p.095502.1-095502.4, Article 095502

2004

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Elastic anisotropy in textured hcp-iron to 112 GPa from sound wave propagation measurements

Earth and planetary science letters, 2004-08, Vol.225 (1), p.243-251

2004

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Melting and pressure-induced amorphization of quartz

Europhysics letters, 1998-06, Vol.42 (6), p.643-648

1998

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The Early Earth: Accretion and Differentiation

1, 2015

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Aggregate and single-crystalline elasticity of hcp cobalt at high pressure

Physical review. B, Condensed matter and materials physics, 2005-10, Vol.72 (13), p.134303.1-134303.7, Article 134303

2005

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Nature of the high-pressure transition in Fe2O3 hematite

Physical review letters, 2002-11, Vol.89 (20), p.205504-205504

2002

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Magnetism in FeO at Megabar Pressures from X-Ray Emission Spectroscopy

Physical review letters, 1999-11, Vol.83 (20), p.4101-4104

1999

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Deformation of (Mg0.9,Fe0.1)SiO3 Perovskite aggregates up to 32 GPa

Earth and planetary science letters, 2003-04, Vol.209 (3-4), p.351-360

2003

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Partitioning of Si and platinum group elements between liquid and solid Fe–Si alloys

Composition of the core from gallium metal–silicate partitioning experiments

Electronic Transitions in Perovskite: Possible Nonconvecting Layers in the Lower Mantle

Low Velocity Zones in the Martian Upper Mantle Highlighted by Sound Velocity Measurements

Iron Partitioning in Earth's Mantle: Toward a Deep Lower Mantle Discontinuity

Investigating Earth's Formation History Through Copper and Sulfur Metal‐Silicate Partitioning During Core‐Mantle Differentiation

Effect of composition, structure, and spin state on the thermal conductivity of the Earth's lower mantle

Reply to Comment by Jennings et al. on “Investigating Earth's Formation History Through Copper and Sulfur Metal‐Silicate Partitioning During Core‐Mantle Differentiation”

Pressure-Induced High-Spin to Low-Spin Transition in FeS Evidenced by X-Ray Emission Spectroscopy

Sound Velocities in Iron to 110 Gigapascals

Elasticity of cobalt at high pressure studied by inelastic X-ray scattering

Electronic properties of transition-metal oxides under high pressure revealed by x-ray emission spectroscopy

Silicon isotopes in angrites and volatile loss in planetesimals

Application of inelastic X-ray scattering to the measurements of acoustic wave velocities in geophysical materials at very high pressure

Synthesis and characterization of a binary noble metal nitride

Oxygen as a light element: A solution to single-stage core formation

Low argon solubility in silicate melts at high pressure

Experimental evidence for a high-pressure isostructural phase transition in osmium

Elastic anisotropy in textured hcp-iron to 112 GPa from sound wave propagation measurements

Melting and pressure-induced amorphization of quartz

The Early Earth: Accretion and Differentiation

Aggregate and single-crystalline elasticity of hcp cobalt at high pressure

Nature of the high-pressure transition in Fe2O3 hematite

Magnetism in FeO at Megabar Pressures from X-Ray Emission Spectroscopy

Deformation of (Mg0.9,Fe0.1)SiO3 Perovskite aggregates up to 32 GPa

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