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Mechanisms and conditions of Ti and Cr incorporation in mantle phlogopite: the results of atomistic simulation

Physics and chemistry of minerals, 2023-03, Vol.50 (1), p.8, Article 8

2023

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Geochemistry of Chromium in the Earth's Mantle

1st ed. 2020., 2019

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Bridgmanite-like crystal structure in the novel Ti-rich phase synthesized at transition zone condition

The American mineralogist, 2017-01, Vol.102 (1), p.227-230

2017

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Interphase REE Partitioning at the Boundary between the Earth’s Transition Zone and Lower Mantle: Evidence from Experiments and Atomistic Modeling

Minerals (Basel), 2020-03, Vol.10 (3), p.262

2020

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Chromium solubility in MgSiO3 ilmenite at high pressure

Physics and chemistry of minerals, 2014-07, Vol.41 (7), p.519-526

2014

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Si-rich Mg-sursassite Mg4Al5Si7O23(OH)5 with octahedrally coordinated Si: A new ultrahigh-pressure hydrous phase

The American mineralogist, 2020-09, Vol.105 (9), p.1432-1435

2020

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X-ray single-crystal and Raman study of knorringite, Mg3(Cr1.58Mg0.21Si0.21)Si3O12, synthesized at 16 GPa and 1,600 °C

Physics and chemistry of minerals, 2014-04, Vol.41 (4), p.267-272

2014

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Incorporation of Ti into the crystal structures of the high-pressure dense silicates anhydrous phase B and superhydrous phase B

Physics and chemistry of minerals, 2019-11, Vol.46 (10), p.909-920

2019

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Discovery of MgTiSi2O7: a new high-pressure silicate with the weberite structure synthesized at transition-zone conditions

Physics and chemistry of minerals, 2017-06, Vol.44 (6), p.419-424

2017

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Incorporation of high amounts of Na in ringwoodite: Possible implications for transport of alkali into lower mantle

The American mineralogist, 2016-02, Vol.101 (2), p.483-486

2016

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Compressibility of two Na-rich clinopyroxenes: A synchrotron single-crystal X-ray diffraction study

The American mineralogist, 2019-06, Vol.104 (6), p.905-913

2019

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Chromium solubility in anhydrous Phase B

Physics and chemistry of minerals, 2016-02, Vol.43 (2), p.103-110

2016

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Chromium solubility in perovskite at high pressure: The structure of (Mg1-xCrx)(Si1-xCrx)O3 (with x = 0.07) synthesized at 23 GPa and 1600 C

The American mineralogist, 2014-04, Vol.99 (4), p.866-869

2014

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Na-bearing majoritic garnet in the Na2MgSi5O12–Mg3Al2Si3O12 join at 11–20 GPa: Phase relations, structural peculiarities and solid solutions

Geochimica et cosmochimica acta, 2013-03, Vol.105, p.1-13

2013

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X-ray single-crystal and Raman study of (Na0.86Mg0.14)(Mg0.57Ti0.43)Si2O6, a new pyroxene synthesized at 7 GPa and 1700 °C

Physics and chemistry of minerals, 2016-11, Vol.43 (10), p.731-738

2016

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Na-bearing majoritic garnet in the Na2MgSi5O12–Mg3Al2Si3O12 join at 11–20GPa: Phase relations, structural peculiarities and solid solutions

Geochimica et cosmochimica acta, 2013-03, Vol.105, p.1-13

2013

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X-ray single-crystal structural characterization of MgCr2O4, a post-spinel phase synthesized at 23GPa and 1600°C

The Journal of physics and chemistry of solids, 2014-05, Vol.75 (5), p.638-641

2014

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Crystal chemistry of sodium in the Earth's interior: The structure of Na2MgSi5O12 synthesized at 17.5 GPa and 1700 C

The American mineralogist, 2011-02, Vol.96 (2-3), p.447-450

2011

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Na-bearing bridgmanite: Synthesis, phase relations and application to the origin of alkaline melts in the uppermost lower mantle

Lithos, 2023-05, Vol.444-445, p.107101, Article 107101

2023

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Synthesis and crystal structures of new high-pressure phases CaAl2O4 and Ca2Al6O11

Lithos, 2020-11, Vol.374-375, p.105689, Article 105689

2020

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The new Ca(Fe,Al)2O4 phase with calcium ferrite-type structure, a likely carrier of Al in the transition zone and lower mantle

The Journal of physics and chemistry of solids, 2022-12, Vol.171, p.111031, Article 111031

2022

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Titanium-rich phases in the Earth's transition zone and lower mantle: Evidence from experiments in the system MgO–SiO2–TiO2(±Al2O3) at 10–24 GPa and 1600 °C

Lithos, 2020-08, Vol.366-367, p.105539, Article 105539

2020

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Structural and chemical characterization of Mg[(Cr,Mg)(Si,Mg)]O 4 , a new post-spinel phase with sixfold-coordinated silicon

The American mineralogist, 2015-07, Vol.100 (7), p.1633-1636

2015

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X-ray single-crystal structural characterization of MgCr sub(2)O sub(4), a post-spinel phase synthesized at 23 GPa and 1600 degree C

The Journal of physics and chemistry of solids, 2014-05, Vol.75 (5), p.638-641

2014

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Partitioning of trace elements between Na-bearing majoritic garnet and melt at 8.5GPa and 1500–1900°C

Lithos, 2014-02, Vol.189, p.159-166

2014

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Mechanisms and conditions of Ti and Cr incorporation in mantle phlogopite: the results of atomistic simulation

Geochemistry of Chromium in the Earth's Mantle

Bridgmanite-like crystal structure in the novel Ti-rich phase synthesized at transition zone condition

Interphase REE Partitioning at the Boundary between the Earth’s Transition Zone and Lower Mantle: Evidence from Experiments and Atomistic Modeling

Chromium solubility in MgSiO3 ilmenite at high pressure

Si-rich Mg-sursassite Mg4Al5Si7O23(OH)5 with octahedrally coordinated Si: A new ultrahigh-pressure hydrous phase

X-ray single-crystal and Raman study of knorringite, Mg3(Cr1.58Mg0.21Si0.21)Si3O12, synthesized at 16 GPa and 1,600 °C

Incorporation of Ti into the crystal structures of the high-pressure dense silicates anhydrous phase B and superhydrous phase B

Discovery of MgTiSi2O7: a new high-pressure silicate with the weberite structure synthesized at transition-zone conditions

Incorporation of high amounts of Na in ringwoodite: Possible implications for transport of alkali into lower mantle

Compressibility of two Na-rich clinopyroxenes: A synchrotron single-crystal X-ray diffraction study

Chromium solubility in anhydrous Phase B

Chromium solubility in perovskite at high pressure: The structure of (Mg1-xCrx)(Si1-xCrx)O3 (with x = 0.07) synthesized at 23 GPa and 1600 C

Na-bearing majoritic garnet in the Na2MgSi5O12–Mg3Al2Si3O12 join at 11–20 GPa: Phase relations, structural peculiarities and solid solutions

X-ray single-crystal and Raman study of (Na0.86Mg0.14)(Mg0.57Ti0.43)Si2O6, a new pyroxene synthesized at 7 GPa and 1700 °C

Na-bearing majoritic garnet in the Na2MgSi5O12–Mg3Al2Si3O12 join at 11–20GPa: Phase relations, structural peculiarities and solid solutions

X-ray single-crystal structural characterization of MgCr2O4, a post-spinel phase synthesized at 23GPa and 1600°C

Crystal chemistry of sodium in the Earth's interior: The structure of Na2MgSi5O12 synthesized at 17.5 GPa and 1700 C

Na-bearing bridgmanite: Synthesis, phase relations and application to the origin of alkaline melts in the uppermost lower mantle

Synthesis and crystal structures of new high-pressure phases CaAl2O4 and Ca2Al6O11

The new Ca(Fe,Al)2O4 phase with calcium ferrite-type structure, a likely carrier of Al in the transition zone and lower mantle

Titanium-rich phases in the Earth's transition zone and lower mantle: Evidence from experiments in the system MgO–SiO2–TiO2(±Al2O3) at 10–24 GPa and 1600 °C

Structural and chemical characterization of Mg[(Cr,Mg)(Si,Mg)]O 4 , a new post-spinel phase with sixfold-coordinated silicon

X-ray single-crystal structural characterization of MgCr sub(2)O sub(4), a post-spinel phase synthesized at 23 GPa and 1600 degree C

Partitioning of trace elements between Na-bearing majoritic garnet and melt at 8.5GPa and 1500–1900°C

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