Physics
Scientist
Rossiiskaia Akademiia Nauk, Institut Geokhimii i Analiticheskoi Khimii, Moscow, Russia
Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, ul. Kosygina 19, Moscow, 117975 Russia
V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry, U.S.S.R. Academy of Sciences, Moscow U.S.S.R.
Department of Earth Sciences, Uppsala University, Villavagen 16, S-752 36 Uppsala, Sweden; V.I.Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, Kosygin Str. 19, 119991 Moscow B-334, Russian Federation
Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, Kosygin Str. 19, 117975, B-334, Moscow, Russia
Department of Earth Sciences, Uppsala University, Uppsala, Sweden
V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, Kosygin Str. 19, 117975 Moscow, B-334, Russia
Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, Moscow, Russia
Theoretical Geochemistry Programme, Institute of Earth Sciences, Uppsala University, Norbyvagen 18B, S-75236 Uppsala, Sweden
Theoretical Geochemistry Programme, Institute of the Earth Sciences, Uppsala University, Norbyvagen 18B, S-75236 Uppsala, Sweden
Vernadskii Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences
V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry, USSR Academy of Sciences, Kosygin str. 19, 117334 Moscow, USSR
V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, 117975 Moscow, Russian Federation
V. I. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, Moscow, Russian Federation.
Chemical Differentiation and Internal Structure of Europa and Callisto
Composition of the Lower Mantle and Origin of the Moon from Interstellar Dust
Constitution of the mantle. 2. Petrological models of transition zone based on FMS phase diagram
Constitution of the mantle. 3. Density, elastic properties and the mineralogy of the 400 km discontinuity
Constitution of the Moon5. Constraints on composition, density, temperature, and radius of a core
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