Works matching IS 00167029 AND DT 2019 AND VI 57 AND IP 9

Results: 10

MgCO3 + SiO2 Reaction at Pressures up to 32 GPa Studied Using in-Situ X-Ray Diffraction and Synchrotron Radiation.

Published in:

Geochemistry International, 2019, v. 57, n. 9, p. 1024, doi. 10.1134/S0016702919090064

By:

Litasov, K. D.;
Shatskiy, A. F.

Publication type:

Article

Synthesis and Raman Spectra of K–Ca Double Carbonates: K2Ca(CO3)2 Bütschliite, Fairchildite, and K2Ca2(CO3)3 at 1 Atm.

Published in:

Geochemistry International, 2019, v. 57, n. 9, p. 981, doi. 10.1134/S0016702919090039

By:

Arefiev, A. V.;
Podborodnikov, I. V.;
Shatskiy, A. F.;
Litasov, K. D.

Publication type:

Article

Texture and Genesis of Polycrystalline Varieties of Diamond Based on Phase-Contrast and Diffraction Contrast Tomography.

Published in:

Geochemistry International, 2019, v. 57, n. 9, p. 1015, doi. 10.1134/S0016702919090106

By:

Shiryaev, A. A.;
Kaminsky, F. V.;
Ludwig, W.;
Zolotov, D. A.;
Buzmakov, A. V.;
Titkov, S. V.

Publication type:

Article

The Compositional Peculiarities of Microinclusions in Diamonds from the Lomonosov Deposit (Arkhangelsk Province).

Published in:

Geochemistry International, 2019, v. 57, n. 9, p. 973, doi. 10.1134/S0016702919090052

By:

Kriulina, G. Yu.;
Iskrina, A. V.;
Zedgenizov, D. A.;
Bobrov, A. V.;
Garanin, V. K.

Publication type:

Article

Melting Relations in the Model Pyrolite at 2.5, 3.0, 7.0 GPa and 1400–1800°C: Application to the Problem of the Formation of High-Chromium Garnets.

Published in:

Geochemistry International, 2019, v. 57, n. 9, p. 988, doi. 10.1134/S0016702919090076

By:

Matrosova, E. A.;
Bendeliani, A. A.;
Bobrov, A. V.;
Kargal'tsev, A. A.;
Ignat'ev, Yu. A.

Publication type:

Article

Formation of Iron Hydride and Iron Carbide from Hydrocarbon Systems at Ultra-High Thermobaric Conditions.

Published in:

Geochemistry International, 2019, v. 57, n. 9, p. 1008, doi. 10.1134/S001670291909009X

By:

Serovaiskii, A. Yu.;
Kolesnikov, A. Yu.;
Kutcherov, V. G.

Publication type:

Article

Evolution of Diamond-Forming Systems of the Mantle Transition Zone: Ringwoodite Peritectic Reaction (Mg,Fe)2SiO4 (Experiment at 20 GPa).

Published in:

Geochemistry International, 2019, v. 57, n. 9, p. 1000, doi. 10.1134/S0016702919090118

By:

Spivak, A. V.;
Litvin, Yu. A.;
Zakharchenko, E. S.;
Simonova, D. A.;
Dubrovinsky, L. S.

Publication type:

Article

SiO2 Inclusions in Sublithospheric Diamonds.

Published in:

Geochemistry International, 2019, v. 57, n. 9, p. 964, doi. 10.1134/S0016702919090131

By:

Zedgenizov, D. A.;
Ragozin, A. L.;
Kagi, H.;
Yurimoto, H.;
Shatsky, V. S.

Publication type:

Article

Reaction between Forsterite and Nitrogen Fluid at High Pressure and High Temperature.

Published in:

Geochemistry International, 2019, v. 57, n. 9, p. 956, doi. 10.1134/S0016702919090040

By:

Kagi, Hiroyuki;
Kubo, Toshinori;
Shinozaki, Ayako;
Okada, Taku;
Ohfuji, Hiroaki;
Nakao, Aiko

Publication type:

Article

Iron and Its Compounds in the Earth's Core: New Data and Ideas.

Published in:

Geochemistry International, 2019, v. 57, n. 9, p. 941, doi. 10.1134/S0016702919090088

By:

Pushcharovsky, D. Yu.

Publication type:

Article

Works matching IS 00167029 AND DT 2019 AND VI 57 AND IP 9

MgCO<sub>3</sub> + SiO<sub>2</sub> Reaction at Pressures up to 32 GPa Studied Using in-Situ X-Ray Diffraction and Synchrotron Radiation.

Synthesis and Raman Spectra of K–Ca Double Carbonates: K<sub>2</sub>Ca(CO<sub>3</sub>)<sub>2</sub> Bütschliite, Fairchildite, and K<sub>2</sub>Ca<sub>2</sub>(CO<sub>3</sub>)<sub>3</sub> at 1 Atm.

Texture and Genesis of Polycrystalline Varieties of Diamond Based on Phase-Contrast and Diffraction Contrast Tomography.

The Compositional Peculiarities of Microinclusions in Diamonds from the Lomonosov Deposit (Arkhangelsk Province).

Melting Relations in the Model Pyrolite at 2.5, 3.0, 7.0 GPa and 1400–1800°C: Application to the Problem of the Formation of High-Chromium Garnets.

Formation of Iron Hydride and Iron Carbide from Hydrocarbon Systems at Ultra-High Thermobaric Conditions.

Evolution of Diamond-Forming Systems of the Mantle Transition Zone: Ringwoodite Peritectic Reaction (Mg,Fe)<sub>2</sub>SiO<sub>4</sub> (Experiment at 20 GPa).

SiO<sub>2</sub> Inclusions in Sublithospheric Diamonds.

Reaction between Forsterite and Nitrogen Fluid at High Pressure and High Temperature.

Iron and Its Compounds in the Earth's Core: New Data and Ideas.