Browsing by Author "Kadik A.A."
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Browsing by Author "Kadik A.A."
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Shilobreyeva S.N.; Kadik A.A.; Minayev V.M.; Kazakov S.S.; Kuz'min L.Y. (1987)The authors determined the amount of carbon in plutonic olivines consisting of single crystals from nodules of ultramafic rocks and mineral phenocrysts in rocks of various origin. The determination of carbon in olivine ...
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Kadik A.A.; Rosenhauer M. (1987)The question of whether subalkalic high-alumina and calcalkalic magnesian basalt: are derived from independent magmas or are the differentiation products of one parental magma has still not been settled. Nor is it clear ...
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Litvin Yu.A.; Litvin V.Yu.; Kadik A.A.; Zharikov V.A. (2006)The formation and evolution of deep-seated carbonatite magmas under the PT conditions of diamond formation represent complex physicochemical processes that incorporate multicomponent silicate material of mantle peridotite, ...
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Kadik A.A. (2003)The application of phase equilibrium methods to the estimation of oxygen fugacity (fO2) showed that the present-day lithospheric and asthenospheric upper mantle layers are moderately oxidized. Their fO 2 values fall above ...
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Kadik A.A.; Lukanin O.A.; Zharkova E.V.; Fel'dman V.I. (2003)For five tektite glasses (moldavites, indochinites, and irgizite), oxygen fugacity (fO2) was measured within the temperature range of 800-1150°C using solid electrochemical cells, and water content was analyzed with FTIR ...
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Kadik A.A. (2006)Oxygen fugacity (fO2) in the Earth's mantle has a bearing on the problems of the chemical differentiation of the Earth's materials and formation of the chemical and phase state of its shells. This paper addresses some ...
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Lukanin O.A.; Lapin I.V.; Kadik A.A. (1990)The authors with alkali basalts of two different compositions, representing different degrees of differentiation, from the same basalt-rhyolite series of Iceland. The experiments were performed in an apparatus in which the ...
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Kadik A.A.; Litvin Yu.A.; Koltashev V.V.; Kryukova E.B.; Plotnichenko V.G. (2006)The solubility of volatile compounds in magmas and the redox state of their mantle source are the main factors that control the transfer of volatile components from the planet's interior to its surface. In theories of the ...
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Lukanin O.A.; Rusakov V.S.; Kotel'nikova A.A.; Kadik A.A. (2002)The effect of pressure on the valence and structural state of iron atoms was experimentally studied at pressures up to 5 kbar in natural basaltic melts under closed system conditions. Basaltic glasses were produced by ...
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