journal article

• Carbonatite metasomatism of peridotite lithospheric mantle: implications for diamond formation and carbonatite-kimberlite magmatism.  Russian Geology and Geophysics.  56:280-295. 2015
• CHROME-RICH GARNETS FROM KIMBERLITES OF YAKUTIA AND THEIR PARAGENESES.  Contributions To Mineralogy and Petrology.  40:39-52.
• Cr-rich rutile: A powerful tool for diamond exploration.  Lithos.  265:304-311.
• Experimental constraints on orthopyroxene dissolution in alkali-carbonate melts in the lithospheric mantle: Implications for kimberlite melt composition and magma ascent.  Chemical Geology.  455:44-56.
• Interaction of peridotite with Ca-rich carbonatite melt at 3.1 and 6.5 GPa: Implication for merwinite formation in upper mantle, and for the metasomatic origin of sublithospheric diamonds with Ca-rich suite of inclusions.  Contributions to Mineralogy and Petrology.  173.
• Melting of kimberlite of the Udachnaya-East pipe: Experimental study at 3–6.5 GPa and 900–1500°C.  Doklady Earth Sciences.  448:200-205.
• Melting phase relations of the Udachnaya-East Group-I kimberlite at 3.0–6.5GPa: Experimental evidence for alkali-carbonatite composition of primary kimberlite melts and implications for mantle plumes.  Gondwana Research.  28:1391-1414.
• Natural occurrence of pure nano-polycrystalline diamond from impact crater.  Scientific Reports.  5:14702.
• Petrogenetic significance of minor elements in olivines from diamonds and peridotite xenoliths from kimberlites of Yakutia.  Lithos.  112:701-713.
• Phase relations and melting in the systems of peridotite-H2O-CO2 and eclogite-H2O-CO2 at pressures up to 27 GPa.  Doklady Earth Sciences.  437:498-502.