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Zapiski RMO (Journal)
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Balitsky V.S. - presentations
personal data: Balitsky, Vladimir Sergeevich
Fedorov session 2016
Growth and morphology of high-germanium quartz single crystals
RMS DPI 2016-1-3-0
RMS Annual Session "Ontogeny of minerals applied to scientific and industrial uses (to the 100 year anniversary of Prof. Dmitry Grigoriev)"
Genetic gemology of crystalline and amorphous varieties of silica
RMS DPI 2009-1-104-0
Mechanisms of formation and morphogenetic types of fluid inclusions in crystals of synthetic minerals
RMS DPI 2009-1-60-0
Professor Dmitry Pavlovich Grigoriev and the role of ontogenic investigations in creation of highly effective technologies of growing of synthetic quartz and its colored varieties
RMS DPI 2009-1-2-0
Stability of topaz and features of silica and alumina transfer in hydrothermal solutions
RMS DPI 2009-1-101-0
Experimental study of the effect of supersaturation and directions of convection streams of solutions on change of growth rates of different faces of quartz crystals
RMS DPI 2009-1-105-0
XIII All-Russian conference on thermobarogeochemistry in conjunction with IV APIFIS symposium
Water-hydrocarbon inclusions in synthetic quartz and questions of formation of oil and other hydrocarbons at interaction of hydrothermal solutions with bituminous and coaly rocks
RMS DPI 2008-1-117-0
Mechanisms of formation and morphogenetic types of fluid inclusions in crystals of synthetic minerals
RMS DPI 2008-1-124-0
2nd International Conference "Crystallogenesis and Mineralogy"
Growth, structural-morphological features and some properties of cobalt tourmaline monocrystals
RMS DPI 2007-1-66-0
Variability of external morphology and internal structure of the quartz crystals grown in hydrothermal solutions in the interval of temperatures of 210-900º and pressure of 40-500 P
RMS DPI 2007-1-33-0
Morphology, composition and aggregate condition of aqueous-hydrocarbonic fluid inclusions in the quartz which has been grown in hydrothermal solutions at presence of oil and bituminous rocks
RMS DPI 2007-1-79-0
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