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Raman spectroscopy of various phosphate minerals and occurrence of tuite in the Elga IIE iron meteorite

Journal of Raman spectroscopy, 2017-11, Vol.48 (11), p.1518-1527

2017

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Melting and subsolidus phase relations in peridotite and eclogite systems with reduced C O H fluid at 3–16 GPa

Earth and planetary science letters, 2014-04, Vol.391, p.87-99

2014

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Solidus of alkaline carbonatite in the deep mantle

Geology (Boulder), 2013-01, Vol.41 (1), p.79-82

2013

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Impact shock origin of diamonds in ureilite meteorites

Proceedings of the National Academy of Sciences - PNAS, 2020-10, Vol.117 (41), p.25310-25318

2020

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The solidus of carbonated eclogite in the system CaO–Al2O3–MgO–SiO2–Na2O–CO2 to 32 GPa and carbonatite liquid in the deep mantle

Earth and planetary science letters, 2010-06, Vol.295 (1-2), p.115-126

2010

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Phonolite-Carbonatite Liquid Immiscibility at 3–6 GPa

Minerals (Basel), 2023-03, Vol.13 (3), p.443

2023

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Formation of Mg-Orthocarbonate through the Reaction MgCO3 + MgO = Mg2CO4 at Earth’s Lower Mantle P–T Conditions

Crystal growth & design, 2021-05, Vol.21 (5), p.2986-2992

2021

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Revision of the CaCO3–MgCO3 phase diagram at 3 and 6 GPa

The American mineralogist, 2018-03, Vol.103 (3), p.441-452

2018

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Phase relations and melting of carbonated peridotite between 10 and 20 GPa: a proxy for alkali- and CO2-rich silicate melts in the deep mantle

Contributions to mineralogy and petrology, 2014-02, Vol.167 (2), p.1, Article 964

2014

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The NaCl-CaCO3 and NaCl-MgCO3 systems at 6 GPa: Link between saline and carbonatitic diamond forming melts

The American mineralogist, 2023-04, Vol.108 (4), p.709-718

2023

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Temperature-induced oligomerization of polycyclic aromatic hydrocarbons at ambient and high pressures

Scientific reports, 2017-08, Vol.7 (1), p.7889-8, Article 7889

2017

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The system NaAlSi2O6‒CaMgSi2O6−CO2 at 3–6.5 GPa: implications for CO2 stability in the eclogitic suite at depths of 100–200 km

Contributions to mineralogy and petrology, 2023-04, Vol.178 (4), p.22, Article 22

2023

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Melt Composition and Phase Equilibria in the Eclogite-Carbonate System at 6 GPa and 900–1500 °C

Minerals (Basel), 2023-01, Vol.13 (1), p.82

2023

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Aragonite-II and CaCO3‑VII: New High-Pressure, High-Temperature Polymorphs of CaCO3

Crystal growth & design, 2017-12, Vol.17 (12), p.6291-6296

2017

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Optical properties of siderite (FeCO 3 ) across the spin transition: Crossover to iron-rich carbonates in the lower mantle

The American mineralogist, 2015-05, Vol.100 (5-6), p.1059-1064

2015

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Looking for “missing” nitrogen in the deep Earth

The American mineralogist, 2017-09, Vol.102 (9), p.1769-1770

2017

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Generation of hydrous-carbonated plumes in the mantle transition zone linked to tectonic erosion and subduction

Tectonophysics, 2015-11, Vol.662, p.454-471

2015

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Carbon precipitation from heavy hydrocarbon fluid in deep planetary interiors

Nature communications, 2013-09, Vol.4 (1), p.2446-2446, Article 2446

2013

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“Kamchatite” diamond aggregate from northern Kamchatka, Russia: New find of diamond formed by gas phase condensation or chemical vapor deposition—Discussion

The American mineralogist, 2020-01, Vol.105 (1), p.141-143

2020

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Crossover from melting to dissociation of CO2 under pressure: Implications for the lower mantle

Earth and planetary science letters, 2011-09, Vol.309 (3-4), p.318-323

2011

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Pyroxene-carbonate reactions in the CaMgSi2O6 ± NaAlSi2O6 + MgCO3 ± Na2CO3 ± K2CO3 system at 3–6 GPa: Implications for partial melting of carbonated peridotite

Contributions to mineralogy and petrology, 2021-05, Vol.176 (5), Article 34

2021

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Enigmatic super-reduced phases in corundum from natural rocks: Possible contamination from artificial abrasive materials or metallurgical slags

Lithos, 2019-09, Vol.340-341, p.181-190

2019

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Coupling between cation and anion disorder in β‐K2Ca3(CO3)4

Journal of applied crystallography, 2024-06, Vol.57 (3), p.665-669

2024

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Ba3(BO3)2: the first example of dynamic disorder in a borate crystal

Physical chemistry chemical physics : PCCP, 2022-07, Vol.24 (27), p.16437-16441

2022

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γ‑BaB2O4: High-Pressure High-Temperature Polymorph of Barium Borate with Edge-Sharing BO4 Tetrahedra

Inorganic chemistry, 2022-01, Vol.61 (4), p.2340-2350

2022

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Raman spectroscopy of various phosphate minerals and occurrence of tuite in the Elga IIE iron meteorite

Melting and subsolidus phase relations in peridotite and eclogite systems with reduced C O H fluid at 3–16 GPa

Solidus of alkaline carbonatite in the deep mantle

Impact shock origin of diamonds in ureilite meteorites

The solidus of carbonated eclogite in the system CaO–Al2O3–MgO–SiO2–Na2O–CO2 to 32 GPa and carbonatite liquid in the deep mantle

Phonolite-Carbonatite Liquid Immiscibility at 3–6 GPa

Formation of Mg-Orthocarbonate through the Reaction MgCO3 + MgO = Mg2CO4 at Earth’s Lower Mantle P–T Conditions

Revision of the CaCO3–MgCO3 phase diagram at 3 and 6 GPa

Phase relations and melting of carbonated peridotite between 10 and 20 GPa: a proxy for alkali- and CO2-rich silicate melts in the deep mantle

The NaCl-CaCO3 and NaCl-MgCO3 systems at 6 GPa: Link between saline and carbonatitic diamond forming melts

Temperature-induced oligomerization of polycyclic aromatic hydrocarbons at ambient and high pressures

The system NaAlSi2O6‒CaMgSi2O6−CO2 at 3–6.5 GPa: implications for CO2 stability in the eclogitic suite at depths of 100–200 km

Melt Composition and Phase Equilibria in the Eclogite-Carbonate System at 6 GPa and 900–1500 °C

Aragonite-II and CaCO3‑VII: New High-Pressure, High-Temperature Polymorphs of CaCO3

Optical properties of siderite (FeCO 3 ) across the spin transition: Crossover to iron-rich carbonates in the lower mantle

Looking for “missing” nitrogen in the deep Earth

Generation of hydrous-carbonated plumes in the mantle transition zone linked to tectonic erosion and subduction

Carbon precipitation from heavy hydrocarbon fluid in deep planetary interiors

“Kamchatite” diamond aggregate from northern Kamchatka, Russia: New find of diamond formed by gas phase condensation or chemical vapor deposition—Discussion

Crossover from melting to dissociation of CO2 under pressure: Implications for the lower mantle

Pyroxene-carbonate reactions in the CaMgSi2O6 ± NaAlSi2O6 + MgCO3 ± Na2CO3 ± K2CO3 system at 3–6 GPa: Implications for partial melting of carbonated peridotite

Enigmatic super-reduced phases in corundum from natural rocks: Possible contamination from artificial abrasive materials or metallurgical slags

Coupling between cation and anion disorder in β‐K2Ca3(CO3)4

Ba3(BO3)2: the first example of dynamic disorder in a borate crystal

γ‑BaB2O4: High-Pressure High-Temperature Polymorph of Barium Borate with Edge-Sharing BO4 Tetrahedra

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