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Dualistic distribution coefficients of trace elements in the system mineral–hydrothermal solution. III. precious metals (Au and Pd) in magnetite and manganmagnetite

Geochemistry international, 2016-02, Vol.54 (2), p.149-166

2016

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Influence of surface nanophases on the processes of crystal formation in multiphase mineral systems

Doklady earth sciences, 2014-03, Vol.455 (1), p.317-322

2014

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Dualistic distribution coefficients of elements in the system mineral-hydrothermal solution. I. Gold accumulation in pyrite

Geochemistry international, 2011-06, Vol.49 (6), p.568-577

2011

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Indicative properties of lazurite as a member of clathrasil mineral family

Doklady earth sciences, 2011-12, Vol.441 (2), p.1732-1737

2011

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Quantitative determination of modes of gold occurrence in minerals by the statistical analysis of analytical data samplings

Geochemistry international, 2008-04, Vol.46 (4), p.423-428

2008

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Dualistic distribution coefficients of elements in the system mineral-hydrothermal solution. II. Gold in magnetite

Geochemistry international, 2012-03, Vol.50 (3), p.227-245

2012

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Surface typochemistry of hydrothermal pyrite: Electron spectroscopic and scanning probe microscopic data. II. Natural pyrite

Geochemistry international, 2009-03, Vol.47 (3), p.231-243

2009

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The effect of the crystal size in sample on the trace-element concentration

Russian geology and geophysics, 2010-07, Vol.51 (7), p.764-773

2010

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Origin of Au-Ag Mineralization in Sphalerite Ores from Data on Sphalerite Co-Crystallization with Ag and Au in Model Hydrothermal Systems

Russian geology and geophysics, 2024-06, Vol.65 (11), p.1302-1315

2024

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Modes of gold occurrence in carbonaceous shales at the patom highland, Eastern Siberia

Geochemistry international, 2011-09, Vol.49 (9), p.942-948

2011

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Mineralogical and isotope-geochemical (δ13C, δ34S and Pb-Pb) characteristics of the Krasniy gold mine (Baikal-Patom Highlands): Constraining ore-forming mechanisms and the model for Sukhoi Log-type deposits

Ore geology reviews, 2020-04, Vol.119, p.103365, Article 103365

2020

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Partitioning and speciation of lanthanides in the system magnetite (hematite) – hydrothermal solution at 450 oC and 100 MPa pressure

Geohimija, 2023-09, Vol.68 (9), p.938-946

2023

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Surface typochemistry of hydrothermal pyrite: Electron spectroscopic and scanning probe microscopic data. I. Synthetic pyrite

Geochemistry international, 2008-06, Vol.46 (6), p.565-577

2008

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Paragenetic relationships between pyrite, carbon, and gold at the Sukhoi Log deposit and typomorphism of the pyrite surface

Doklady earth sciences, 2009-06, Vol.426 (1), p.690-694

2009

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The nature of the stability of an incommensurate 3D structural modulation in Baikal lazurite: Experimental data at 550°C

Geochemistry international, 2009-08, Vol.47 (8), p.815-830

2009

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Modulated cubic lazurite from the Baikal region: Structure transformed to the state of forced equilibrium

Doklady earth sciences, 2010-07, Vol.433 (1), p.931-936

2010

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Distribution of heavy-metal (Hg, Cd, and Pb) chemical species between pyrite and hydrothermal solution

Geochemistry international, 2010-06, Vol.48 (6), p.611-616

2010

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Mechanisms and species of gold incorporation into crystals of cadmium, lead, and iron sulfides

Russian geology and geophysics, 2008-08, Vol.49 (8), p.594-601

2008

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Partition of heavy metals (Hg, Cd, and Pb) between sphalerite and hydrothermal solution and the typomorphism of sphalerite surface: XPS, AES, and AFM data

Geochemistry international, 2010-01, Vol.48 (1), p.94-105

2010

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The First Application of Palladium–Phosphorus Catalysts in the Direct Synthesis of Hydrogen Peroxide: Reasons for the Promoting Action of Phosphorus

Kinetika i kataliz, 2023-11, Vol.64 (6), p.749-760

2023

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A Study of Cadmium Incorporation into Pyrrhotites of Different Stoichiometry

Geochemistry international, 2004-02, Vol.42 (2), p.115-115

2004

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Nonautonomous nanophase on a hydrothermal pyrite surface and its geochemical significance

Doklady earth sciences, 2008-12, Vol.423 (2), p.1501-1506

2008

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Mechanism of au incorporation into Cd sulfide: Evidence from Au partition between CdS and Ag2S

Geochemistry international, 2007-11, Vol.45 (11), p.1146-1151

2007

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Nonautonomous phases as potential sources of incompatible elements

Doklady earth sciences, 2006-02, Vol.407 (1), p.280-283

2006

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Using cocrystallization coefficients of isomorphous admixtures for determination of element concentrations in ore-forming solutions (by the example of Mn/Fe ratio in magnetite)

Russian geology and geophysics, 2015-08, Vol.56 (8), p.1128-1132

2015

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Dualistic distribution coefficients of trace elements in the system mineral–hydrothermal solution. III. precious metals (Au and Pd) in magnetite and manganmagnetite

Influence of surface nanophases on the processes of crystal formation in multiphase mineral systems

Dualistic distribution coefficients of elements in the system mineral-hydrothermal solution. I. Gold accumulation in pyrite

Indicative properties of lazurite as a member of clathrasil mineral family

Quantitative determination of modes of gold occurrence in minerals by the statistical analysis of analytical data samplings

Dualistic distribution coefficients of elements in the system mineral-hydrothermal solution. II. Gold in magnetite

Surface typochemistry of hydrothermal pyrite: Electron spectroscopic and scanning probe microscopic data. II. Natural pyrite

The effect of the crystal size in sample on the trace-element concentration

Origin of Au-Ag Mineralization in Sphalerite Ores from Data on Sphalerite Co-Crystallization with Ag and Au in Model Hydrothermal Systems

Modes of gold occurrence in carbonaceous shales at the patom highland, Eastern Siberia

Mineralogical and isotope-geochemical (δ13C, δ34S and Pb-Pb) characteristics of the Krasniy gold mine (Baikal-Patom Highlands): Constraining ore-forming mechanisms and the model for Sukhoi Log-type deposits

Partitioning and speciation of lanthanides in the system magnetite (hematite) – hydrothermal solution at 450 oC and 100 MPa pressure

Surface typochemistry of hydrothermal pyrite: Electron spectroscopic and scanning probe microscopic data. I. Synthetic pyrite

Paragenetic relationships between pyrite, carbon, and gold at the Sukhoi Log deposit and typomorphism of the pyrite surface

The nature of the stability of an incommensurate 3D structural modulation in Baikal lazurite: Experimental data at 550°C

Modulated cubic lazurite from the Baikal region: Structure transformed to the state of forced equilibrium

Distribution of heavy-metal (Hg, Cd, and Pb) chemical species between pyrite and hydrothermal solution

Mechanisms and species of gold incorporation into crystals of cadmium, lead, and iron sulfides

Partition of heavy metals (Hg, Cd, and Pb) between sphalerite and hydrothermal solution and the typomorphism of sphalerite surface: XPS, AES, and AFM data

The First Application of Palladium–Phosphorus Catalysts in the Direct Synthesis of Hydrogen Peroxide: Reasons for the Promoting Action of Phosphorus

A Study of Cadmium Incorporation into Pyrrhotites of Different Stoichiometry

Nonautonomous nanophase on a hydrothermal pyrite surface and its geochemical significance

Mechanism of au incorporation into Cd sulfide: Evidence from Au partition between CdS and Ag2S

Nonautonomous phases as potential sources of incompatible elements

Using cocrystallization coefficients of isomorphous admixtures for determination of element concentrations in ore-forming solutions (by the example of Mn/Fe ratio in magnetite)

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