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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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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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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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Phonolite-Carbonatite Liquid Immiscibility at 3–6 GPa

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

2023

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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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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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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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Change in carbonate budget and composition during subduction below metal saturation boundary

Di xue qian yuan., 2023-01, Vol.14 (1), p.101463, Article 101463

2023

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The System KCl–CaCO3–MgCO3 at 3 GPa

Minerals (Basel), 2023-02, Vol.13 (2), p.248

2023

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Noncentrosymmetric Na2Ca4(CO3)5 Carbonate of “M13M23XY3Z” Structural Type and Affinity between Borate and Carbonate Structures for Design of New Optical Materials

Crystal growth & design, 2017-11, Vol.17 (11), p.6079-6084

2017

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High-Pressure–High-Temperature Study of Benzene: Refined Crystal Structure and New Phase Diagram up to 8 GPa and 923 K

Crystal growth & design, 2018-05, Vol.18 (5), p.3016-3026

2018

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Natural occurrence of pure nano-polycrystalline diamond from impact crater

Scientific reports, 2015-10, Vol.5 (1), p.14702-14702, Article 14702

2015

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Quench Products of K-Ca-Mg Carbonate Melt at 3 and 6 GPa: Implications for Carbonatite Inclusions in Mantle Minerals

Minerals (Basel), 2022-09, Vol.12 (9), p.1077

2022

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Oligomerization and carbonization of polycyclic aromatic hydrocarbons at high pressure and temperature

Carbon (New York), 2015-04, Vol.84, p.225-235

2015

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New High-Pressure Structures of Transition Metal Carbonates with O3C–CO3 Orthooxalate Groups

Symmetry (Basel), 2023-02, Vol.15 (2), p.421

2023

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Genetic link between saline and carbonatitic mantle fluids: The system NaCl-CaCO3-MgCO3 ± H2O ± Fe0 at 6 GPa

Di xue qian yuan., 2022-11, Vol.13 (6), p.101431, Article 101431

2022

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Cuboctahedral type Ib diamonds in ophiolitic chromitites and peridotites: the evidence for anthropogenic contamination

High pressure research, 2019-07, Vol.39 (3), p.480-488

2019

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High‐pressure phases of sulfur: Topological analysis and crystal structure prediction

physica status solidi (b), 2017-07, Vol.254 (7), p.n/a

2017

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Jadeite in Chelyabinsk meteorite and the nature of an impact event on its parent body

Scientific reports, 2014-05, Vol.4 (1), p.5033-5033, Article 5033

2014

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Fe-Ni-P-S Melt Pockets in Elga IIE Iron Meteorite: Evidence for the Origin at High-Pressures Up to 20 GPa

Minerals (Basel), 2019-10, Vol.9 (10), p.616

2019

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Synthesis of heavy hydrocarbons at the core-mantle boundary

Scientific reports, 2015-12, Vol.5 (1), p.18382-18382, Article 18382

2015

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The System K2CO3–CaCO3–MgCO3 at 3 GPa: Implications for Carbonatite Melt Compositions in the Shallow Continental Lithosphere

Minerals (Basel), 2019-05, Vol.9 (5), p.296

2019

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The Mg-carbonate–Fe interaction: Implication for the fate of subducted carbonates and formation of diamond in the lower mantle

Di xue qian yuan., 2019-07, Vol.10 (4), p.1449-1458

2019

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Toward Analysis of Structural Changes Common for Alkaline Carbonates and Binary Compounds: Prediction of High-Pressure Structures of Li2CO3, Na2CO3, and K2CO3

Crystal growth & design, 2016-10, Vol.16 (10), p.5612-5617

2016

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The K2CO3–CaCO3–MgCO3 System at 6 GPa: Implications for Diamond Forming Carbonatitic Melts

Minerals (Basel), 2019-09, Vol.9 (9), p.558

2019

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

Impact shock origin of diamonds in ureilite meteorites

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

Phonolite-Carbonatite Liquid Immiscibility at 3–6 GPa

Carbon precipitation from heavy hydrocarbon fluid in deep planetary interiors

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

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

Change in carbonate budget and composition during subduction below metal saturation boundary

The System KCl–CaCO3–MgCO3 at 3 GPa

Noncentrosymmetric Na2Ca4(CO3)5 Carbonate of “M13M23XY3Z” Structural Type and Affinity between Borate and Carbonate Structures for Design of New Optical Materials

High-Pressure–High-Temperature Study of Benzene: Refined Crystal Structure and New Phase Diagram up to 8 GPa and 923 K

Natural occurrence of pure nano-polycrystalline diamond from impact crater

Quench Products of K-Ca-Mg Carbonate Melt at 3 and 6 GPa: Implications for Carbonatite Inclusions in Mantle Minerals

Oligomerization and carbonization of polycyclic aromatic hydrocarbons at high pressure and temperature

New High-Pressure Structures of Transition Metal Carbonates with O3C–CO3 Orthooxalate Groups

Genetic link between saline and carbonatitic mantle fluids: The system NaCl-CaCO3-MgCO3 ± H2O ± Fe0 at 6 GPa

Cuboctahedral type Ib diamonds in ophiolitic chromitites and peridotites: the evidence for anthropogenic contamination

High‐pressure phases of sulfur: Topological analysis and crystal structure prediction

Jadeite in Chelyabinsk meteorite and the nature of an impact event on its parent body

Fe-Ni-P-S Melt Pockets in Elga IIE Iron Meteorite: Evidence for the Origin at High-Pressures Up to 20 GPa

Synthesis of heavy hydrocarbons at the core-mantle boundary

The System K2CO3–CaCO3–MgCO3 at 3 GPa: Implications for Carbonatite Melt Compositions in the Shallow Continental Lithosphere

The Mg-carbonate–Fe interaction: Implication for the fate of subducted carbonates and formation of diamond in the lower mantle

Toward Analysis of Structural Changes Common for Alkaline Carbonates and Binary Compounds: Prediction of High-Pressure Structures of Li2CO3, Na2CO3, and K2CO3

The K2CO3–CaCO3–MgCO3 System at 6 GPa: Implications for Diamond Forming Carbonatitic Melts

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