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au.\*:("GANEEV IG")

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PROPRIETES DES SOLUTIONS HYDROTHERMALES ET FORMES DE MIGRATION DES SUBSTANCES MINERALESGANEEV IG.1976; DOKL. AKAD NAUK S.S.S.R.; S.S.S.R.; 1976, VOL. 227, NUM. 0002, P. 458 A 460Serial Issue

QUELQUES ASPECTS CHIMIQUES DE LA CROISSANCE HYDROTHERMALE DES CRISTAUXGANEEV IG.1975; DOKL. AKAD NAUK S.S.S.R.; S.S.S.R.; DA. 1975; VOL. 223; NO 5; PP. 1119-1121; BIBL. 7 REF.Article

MODE OF ORIGIN OF THE HEAVY PHASE IN THE HYDROTHERMAL GROWTH OF QUARTZ.GANEEV IG.1968; DOKL. EARTH SCI. SECT.; USA; 1968(8), VOL. 181, P. 193 A 194Miscellaneous

ON THE DISSOLUTION MECHANISM AND MIGRATION FORMS OF SILICA IN ALKALINE HYDROTHERMAL SOLUTIONS.GANEEV IG.1968; GEOKHIMIJA; SUN; 1968(6), NUM. 0006, P. 727 A 729Miscellaneous

ON THE MECHANISM OF SOLUTION OF SILICA AND THE FORMS OF ITS TRANSPORT IN HYDROTHERMAL SOLUTIONS (ABSTRACT).GANEEV IG.1968; GEOCHEM. INTERNATION.; USA; 1968, VOL. 5, NUM. 0003Miscellaneous

NEKOTORYE KHIMICHESKIE ASPEKTY GIDROTERMAL' NOGO VYRASHCHIVANIYA KRISTALLOV I PRIRODNOGO MINERALOOBRAZOVANIYA = QUELQUES ASPECTS CHIMIQUES DE LA CROISSANCE HYDROTHERMALE DES CRISTAUX ET DE LA MINERALOGENESE NATURELLEGANEEV IG.1980; NEODNORODNOST' MINERALOV I ROST KRISTALLOV. S'' EZDA MMA. 11/1978/NOVOSIBIRSK; SUN; MOSKVA: NAUKA; DA. 1980; PP. 186-194; ABS. ENG; 2 TAB. ; TABL./ILL.Conference Paper

STRUCTURE ET PROPRIETES DES SOLUTIONS DE SILICATESGANEEV IG.1974; GEOKHIMIJA; SUN; 1974, NUM. 0003, P. 434 A 443Serial Issue

LE GRADIENT THERMIQUE FACTEUR DE LA DIFFERENCIATION DES FLUIDES HYDROTHERMAUX, LA ZONALITE ET REPARTITION VERTICALE DES FILONS QUARTZITIQUES MOLYBDENITIQUES ET WOLFRAMITIQUESGANEEV IG; POKALOV VT.1975; DOKL. AKAD. NAUK S.S.S.R.; SUN; 1975, VOL. 220, NUM. 0003, P. 690 A 693Serial Issue

STRUCTURE AND PROPERTIES OF SILICATE MELTS.GANEYEV IG; GANEEV IG.1975; GEOCHEM. INTERNATION.; USA; DU RUSSE: GEOKHIMIJA, S.S.S.R. 1974; NO 3, 434-443,1975, VOL. 11, NUM. 0002, P. 329 A 337Miscellaneous

GEOCHEMISTRY OF THE LATERITE PROCESS (PHYSICOCHEMICAL ASPECT OF THE REMOVAL OF SILICA DURING LATERIZATION).TENYAKOV VA; GANEEV IG.sdLITHOL. MINER. RESOURCES; U.S.A.; DU RUSSE: LITOL. POLEZN. ISKOPAEM., S.S.S.S.R. 1975; NO 2, 56-62,1975, VOL. 10, NUM. 0002, P. 187 A 192Miscellaneous

ASPECTS PHYSICOCHIMIQUES DE LA CROISSANCE HYDROTHERMALE DES CRISTAUXGANEEV IG; RUMYANTSEV VN.1977; KRISTALLOGRAFIJA; S.S.S.R.; DA. 1977; VOL. 22; NO 1; PP. 162-167; BIBL. 9 REF.Article

MIGRATION OF SILICA IN HYDROTHERMAL SOLUTIONS.GANEYEV IG; GANEEV IG.sdDOKL. EARTH SCI. SECT.; U.S.A.; DU RUSSE: DOKL. AKAD. NAUK S.S.S.R., S.S.S.R. 1974; 214, NO 5, 1175-1178,1974, VOL. 214, P. 216 A 218Miscellaneous

GEOCHIMIE DU PROCESSUS LATERITIQUE. ASPECT PHYSICO-CHIMIQUE DU DEPART DE LA SILICE AU COURS DE LA LATERITISATIONTENYAKOV VA; GANEEV IG.1975; LITOL. POLEZN. ISKOPAEM.; S.S.S.R.; 1975, NUM. 0002, P. 56 A 62Serial Issue

SUR LE COMPORTEMENT DU SULFURE DE CADMIUM DANS DES CONDITIONS HYDROTHERMALES.DRONOV AV; GANEEV IG.1968; GEOL. RUDN. MESTOROZHD; SUN; 1968, VOL. 10, NUM. 0006, P. 87 A 94Miscellaneous

ROLE DE LA DENSITE DE LA SOLUTION LORS DE LA CRISTALLISATION HYDROTHERMALE DU QUARTZRUMYANTSEV VN; GANEEV IG.1978; DOKL. AKAD. NAUK S.S.S.R.; SUN; DA. 1978; VOL. 243; NO 5; PP. 1168-1170; BIBL. 6 REF.Article

PROPERTIES OF HYDROTHERMAL SOLUTIONS AND THE FORM IN WHICH MINERAL COMPONENTS ARE TRANSPORTED IN THEM.GANEYEV IG; GANEEV IG.1976; DOKL. EARTH SCI. SECT.; U.S.A.; DA. 1976; VOL. 227; PP. 205-207; BIBL. 9 REF.; 1 ILL.; DU RUSSE: DOKL. AKAD. NAUK S.S.S.R., S.S.S.R. 1976; 227, NO 2, 458-460Article

SOME PROPERTIES OF H2O AT ELEVATED PRESSURES AND TEMPERATURES.GANEEV IG; RUMJANCEV VN.1969; GEOKHIMIJA; SUN; 1969, NUM. 0007, P. 881 A 890Miscellaneous

EHKSPERIMENTAL'NOE MODELIROVANIE METAMORFIZMA SIDERITOSODERZHASHCHIKH POROD = MODELISATION EXPERIMENTALE DU METAMORPHISME DE ROCHES A SIDERITEGANEEV IG; KOTINA RP; MALINOVSKAYA EK et al.1981; PROBL. OSAD. GEOL. DOKEMBR.; ISSN 547271; SUN; DA. 1981; NO 6; PP. 131-133; BIBL. 2 REF.; IGCP-91; ILL.Article

PARTICULARITES DE LA SOLUBILITE DU CORINDON DANS LES SOLUTIONS ALCALINES A HAUTE TEMPERATUREGANEEV IG; MENKOVSKIJ MA; RUMYANTSEV VN et al.1974; IZVEST. AKAD. NAUK S.S.S.R., NEORG. MATER.; S.S.S.R.; DA. 1974; VOL. 10; NO 12; PP. 2163-2165; BIBL. 6 REF.Article

THE EFFECT OF TEMPERATURE GRADIENT ON DIFFERENTIATION OF HYDROTHERMAL SOLUTIONS, ZONING OF WOLFRAMITE-MOLYBDENITE-QUARTZ VEINS AND THEIR VERTICAL EXTENT.GANEYEV IG; GANEEV IG; POKALOV VT et al.sdDOKL. EARTH SCI. SECT.; U.S.A.; DU RUSSE: DOKL. AKAD. NAUK S.S.S.R., S.S.S.R. 1975; 220, NO 3, 690-693,1975, VOL. 220, P. 188 A 190Miscellaneous

THERMODYNAMIC PROPERTIES OF MACEDONITE (ALPHA -PBTIO3) AND THE CONDITIONS OF ITS FORMATION IN HYDROTHERMAL VEINS.TUGARINOV IA; GANEYEV IG; GANEEV IG et al.1975; GEOCHEM. INTERNATION.; U.S.A.; DA. 1975; VOL. 12; NO 4; PP. 47-53; BIBL. 2 P.; 3 ILL.; DU RUSSE: GEOKHIMIJA, S.S.S.R. 1975; NO 7, 1021-1028Article

EXPERIMENTAL DETERMINATION OF HYDROLYSIS CONSTANTS OF LEAD IONS IN AQUEOUS SOLUTIONS AT TEMPERATURES UP TO 300OC.TUGARINOV IA; GANEYEV IG; GANEEV IG et al.1975; GEOCHEM. INTERNATION.; U.S.A.; DA. 1975; VOL. 12; NO 5; PP. 47-55; BIBL. 27 REF.; 8 ILL.; DU RUSSE: GEOKHIMIJA, S.S.S.R. 1975; NO 9, 1345-1354Article

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