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STABILITY OF MERWINITE IN THE SYSTEM CAO-MGO-SIO2-CO2.SHMULOVICH KI.1969; DOKL. EARTH SCI. SECT.; USA; 1969, VOL. 184, P. 125 A 127Miscellaneous

STABILITY OF LARNITE IN THE CAO-SIO2-CO2 SYSTEM.SHMULOVICH KI.1967; DOKL. EARTH SCI. SECT.; USA; 1967, VOL. 177, P. 142 A 145Miscellaneous

STABILITE DE LA MERWINITE DANS LE SYSTEME CAO-MGO-SIO2-CO2.SHMULOVICH KI.1969; DOKL. AKAD. NAUK S.S.S.R.; SUN; 1969, VOL. 184, NUM. 0005, P. 1177 A 1179Miscellaneous

PHASE EQUILIBRIA IN THE CAO-AI2O3-SIO2-CO2 SYSTEM.SHMULOVICH KI.sdGEOCHEM. INTERNATION.; U.S.A.; DU RUSSE: GEOKHIMIJA, S.S.S.R. 1974; NO 8, 1272-1277,1974, VOL. 11, NUM. 0004, P. 883 A 887Miscellaneous

ETUDE EXPERIMENTALE DES EQUILIBRES DE PHASES DANS LE SYSTEME CAO-AL2O3-SIO2-COSHMULOVICH KI.1974; GEOKHIMIJA; SUN; 1974, NUM. 0008, P. 1272 A 1277Serial Issue

REPARTITION DES OXIDES D'ELEMENTS PETROGENES DANS LES EFFUSIONS CONTEMPORAINES DES ILES KOURILLES.SHMULOVICH KI.1966; SOVREMENNYJ.VULKANIZM.2.VSESOJUZNOE.VULKANOLOGICHESKOE.SOVESHCHANIE.PE TROPAVLOVSK-KAMCHATSKIJ.1964.1.MOSKVA.IZDAT.NAUKA.; 1966, P. 264 A 270Miscellaneous

EXPERIMENTAL STUDY OF THE SYSTEM CAO-SIO2-CO2 BETWEEN 800-1100 DEGREES AND AT PCO2=50-500 KG/CM2.ZHARIKOV VA; SHMULOVICH KI.1969; DOKL. EARTH SCI. SECT.; USA; 1969, VOL. 188, P. 170 A 173Miscellaneous

ACTIVATION DU CO2, PAR DES ELECTROLYTES, AU-DESSUS D'UN POINT CRITIQUE DANS DES SOLUTIONS AQUEUSESSHMULOVICH KI; KOTOVA NP.1980; DOKL. AKAD. NAUK SSSR; ISSN 0002-3264; SUN; DA. 1980; VOL. 253; NO 4; PP. 952-956; BIBL. 11 REF.; ILL.Article

FUGACITY COEFFICIENTS FOR CO2 FROM 10132 TO 10000 BAR AND 450-1300O K.SHMULOVICH KI; SHMONOV VM.1975; GEOCHEM. INTERNATION.; U.S.A.; DA. 1975; VOL. 12; NO 2; PP. 202-206; BIBL. 12 REF.; 2 ILL.; DU RUSSE: GEOKHIMIJA, S.S.S.R. 1975; NO 4, 551-555Article

HIGH-TEMPERATURE MINERAL EQUILIBRIA IN THE CAO-SIO2-CO2 SYSTEM.ZHARIKOV VA; SHMULOVICH KI.1969; GEOKHIMIJA; SUN; 1969(9), NUM. 0009, P. 1039 A 1056Miscellaneous

MOLAL VOLUMES AND EQUATION OF STATE OF CO2 AT TEMPERATURES FROM 100 TO 1000OC AND PRESSURES FROM 2000 TO 10000 BARS.SHMONOV VM; SHMULOVICH KI.sdDOKL. EARTH SCI. SECT.; U.S.A.; DU RUSSE: DOKL. AKAD. NAUK S.S.S.R., S.S.S.R. 1974; 217, NO 4, 935-938,1974, VOL. 217, P. 206 A 209Miscellaneous

REACTION DE CARBONATATION DES PYROXENES DE LA SERIE DIOPSIDE-HEDENBERGITEKHODOREVSKAYA LI; SHMULOVICH KI.1980; OCESKI FIZ.-HIM. PETROL.; ISSN 0320-6386; SUN; DA. 1980; NO 9; PP. 184-189; BIBL. 15 REF.; 47 ANAL.; 1 TAB. ; ANAL./TABL.Article

COEFFICIENTS DE FUGACITE DE CO2 DE 1,0132 A 10000 BAR ET DE 450 A 1300 KSHMULOVICH KI; SHMONOV VM.1975; GEOKHIMIJA; S.S.S.R.; DA. 1975; NO 4; PP. 551-555; ABS. ANGL.; BIBL. 12 REF.; 2 ILL.Article

ETUDE EXPERIMENTALE DU SYSTEME CAO-SIO2-CO2 A 800-1100 DEGRES C ET SOUS 50-500 KG/CM2 DE PRESSION DE CO2.ZHARIKOV VA; SHMULOVICH KI.1969; DOKL. AKAD. NAUK S.S.S.R.; SUN; 1969(10), VOL. 188, NUM. 0006, P. 1364 A 1367Miscellaneous

EXPERIMENTAL STUDIES IN THE SYSTEM CAO-MGO-AL2O3-SIO2-CO2-H2O AND CONDITIONS OF HIGH-TEMPERATURE METAMORPHISM.ZHARIKOV VA; SHMULOVICH KI; BULATOV VK et al.1977; TECTONOPHYSICS; NETHERL.; DA. 1977; VOL. 43; NO 1-2; PP. 145-162; BIBL. 2 P.; 7 ILL.Article

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