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ESSAI DE CLASSIFICATION PRELIMINAIRE DES METASOMATITES ENCAISSANTES HYPOTHERMAUXSHCHERBAN IP.1976; TRUDY INST. GEOL. GEOFIZ., MOSKVA; S.S.S.R.; DA. 1976; NO 376; PP. 210-216; BIBL. 16 REF.Article

POSITION DE LA LIMITE THERMIQUE ENTRE LES FORMATIONS DE ROCHES METASOMATIQUES DE BASSE TEMPERATURE ET DE MOYENNE TEMPERATURE.SHCHERBAN+ IP.1971; DOKL. AKAD. NAUK S.S.S.R.; SUN; 1971(5), VOL. 198, NUM. 0001, P. 194 A 197Miscellaneous

MODE OF ORIGIN OF FLUORITE IN ASSOCATION WITH SILICA.SHCHERBAN' IP.1968; DOKL. EARTH SCI. SECT.; USA; 1968(11), VOL. 178, P. 197 A 199Miscellaneous

SOME POSSIBLE FORMS OF MIGRATION OF SILICON IN AQUEOUS SOLUTION AND THE MODE OF ORIGIN OF SILICA.SHCHERBAN IP.1967; DOKL. EARTH SCI. SECT.; USA; 1967, VOL. 177, P. 241 A 243Miscellaneous

O VYSOKOTEMPERATURNYKH FORMATSIYAKH OKOLORUDNYKH METASOMATITOV = METASOMATITES DE HAUTE TEMPERATURESHCHERBAN' IP.1983; DOKL. AKAD. NAUK. SSSR; ISSN 0002-3264; SUN; DA. 1983; VOL. 268; NO 1; PP. 180-184; BIBL. 7 REF.; ILL.Article

USLOVIYA OBRAZOVANIYA NIZKOTEMPERATURNYKH OKOLORUDNYKH METASOMATITOV. (NA PRIMERE ALTAE-SAYANSKOJ OBLASTI). = CONDITIONS DE FORMATION A BASSE TEMPERATURE DES ROCHES ENCAISSANTES METASOMATIQUES D'APRES L'EXEMPLE DE LA REGION D'ALTAI-SAIANSHCHERBAN IP.1975; NOVOSIBIRSK NAUKA; 1975, P. 1 A 200Book

O KHLORIT-ORTOKLAZOVYKH OKOLORUDNYKH METASOMATITAKH NA URANOVYKH RUDOPROYAVLENIYAKH = ROCHES METASOMATIQUES A CHLORITE ET ORTHOCLASE DES EPONTES D'INDICES D'URANIUMSHCHERBAN' IP; SHUN'KO VV.1983; GEOL. RUDN. MESTOROZD.; ISSN 0016-7770; SUN; DA. 1983; VOL. 25; NO 3; PP. 43-54; BIBL. 1 P.; 4 TAB. ; COUPE GEOL./ILL./TABL.Article

ETUDE EXPERIMENTALE DE LA STABILITE DE L'ASSOCIATION DOLOMIE+ SILICE DANS DES CONDITIONS HYDROTHERMALES.SHCHERBAN' IP; SHIROKIKH IN.1971; GEOL. I GEOFIZ.; SUN; 1971, NUM. 0002, P. 119 A 122Miscellaneous

ON QUANTITATIVE ESTIMATION OF THE TEMPERATURE FIELDS,WHICH ORIGINATED BY THE MOVEMENT OF HYDROTHERMAL SOLUTIONS IN THE FISSURE CHANNELS.SHIROKIKH IN; SHCHERBAN IP.1968; AKAD. NAUK S.S.S.R., SIB. OTD., GEOL. GEOFIZ ; SUN; 1968(6), NUM. 0006, P. 132 A 137Miscellaneous

DONNEES EXPERIMENTALES ET THERMODYNAMIQUES SUR LA STABILITE DU GYPSE, DU SEMIHYDRATE ET DE L'ANHYDRITE DANS LES CONDITIONS HYDRO-THERMALES.SHCHERBAN+ IP; SHIROKIKH IN.1970; AKAD. NAUK S.S.S.R., SIB. OTD., GEOL. GEOFIZ ; SUN; 1970(9), NUM. 0009, P. 102 A 105Miscellaneous

GENETIC TYPES OF SILICIFICATED ROCKS OF SOUTH-EASTERN ALTAI AND THEIR PROSPECTING SIGNIFICANCE.SHCHERBAN' IP; OBOLENSKIJ AA.1967; AKAD. NAUK S.S.S.R., SIB. OTD., GEOL. GEOFIZ ; SUN; 1967(6), NUM. 0006, P. 40 A 49Miscellaneous

PRO DVA TIPI KOLORUDNIKH KVARTSITIV = TWO TYPES OF NEAR-ORE QUARTZITES = DEUX TYPES DE QUARTZITES PROCHES DE MINERAISSHCHERBAN' IP; GUSARENKO LO.1981; DOPOV. AKAD. NAUK UKR. RSR, SER. B: GEOL. KHIM. BIOL. NAUKI; ISSN 0002-3523; SUN; DA. 1981; VOL. 1981; NO 7; PP. 37-39; ABS. ENG; BIBL. 9 REF.; ILL.Article

MISE EN MODELE DU PROCESSUS DE REMPLACEMENT METASOMATIQUE DE LA CALCITE PAR LE GYPSE DANS DES CONDITIONS STANDARD.SHCHERBAN IP; SHIROKIKH IN.1971; GEOL. I GEOFIZ.; SUN; 1971, NUM. 0005, P. 148 A 151Miscellaneous

CALCULS THERMODYNAMIQUES POUR QUELQUES REACTIONS DANS LE SYSTEME MGO-CAO-CO2-H20 DANS LES CONDITIONS NORMALES ET HYDROTHERMALES.SHCHERBAN+ IP; BOROVIKOVA GA.1970; AKAD. NAUK S.S.S.R., SIB. OTD., GEOL. GEOFIZ ; SUN; 1970, VOL. 126, NUM. 0006, P. 21 A 28Miscellaneous

ANALYSE THERMODYNAMIQUE DE QUELQUES REACTIONS POSSIBLES AU COURS DE LA METASOMATOSE ACIDE ET BASIQUESHCHERBAN IP; BOROVIKOVA GA.1972; ZAP. VSESOJUZ. MINERAL. OBSHCHEST.; S.S.S.R. ; 1972, VOL. 101, NUM. 0004, P. 404 A 412Serial Issue

GENETIC TYPES OF SILICIFICATED ROCKS OF SOUTH-EASTERN ALTAI AND THEIR PROSPECTING SIGNIFICANCE.SHCHERBAN' IP; OBOLENSKIJ AA.1967; AKAD. NAUK S.S.S.R., SIB. OTD., GEOL. GEOFIZ ; SUN; 1967(6), NUM. 0006, P. 40 A 49Miscellaneous

PROCESSUS DES CONDITIONS PHYSICO-CHIMIQUES DE FORMATION DES QUARTZITES SECONDAIRESSHCHERBAN IP; BOROVIKOVA GA.1977; GEOL. I GEOFIZ.; S.S.S.R.; DA. 1977; NO 2; PP. 144-148; ABS. ANGL.; BIBL. 4 REF.Article

DONNEES THERMODYNAMIQUES SUR LES CONDITIONS DE FORMATION DES LISTVENITES ET DES ROCHES LISTVENITISEES.SHCHERBAN' IP; BOROVIKOVA GA.1970; DOKL. AKAD. NAUK S.S.S.R.; SUN; 1970(4), VOL. 191, NUM. 0006, P. 1389 A 1392Miscellaneous

SUR UN NOUVEAU TYPE DE METASOMATITES DANS DES GISEMENTS-PYRITO-POLYMETALLIQUESSHCHERBAN IP; SHIROKIKH IN.1977; DOKL. AKAD NAUK S.S.S.R.; S.S.S.R.; DA. 1977; VOL. 235; NO 2; PP. 458-461; BIBL. 4 REF.; 12 ANAL.Article

THERMODYNAMIC AND EXPERIMENTAL DATA ON STABILITY OF GYPSUM, HEMIHYDRATE, AND ANHYDRITE UNDER HYDROTHERMAL CONDITIONS.SHCHERBAN' IP; SHIROKIKH IN.1971; INTERNATION. GEOL. REV.; SUN; 1971, VOL. 13, NUM. 0011, P. 1671 A 1673Miscellaneous

EXPERIMENTAL DATA ON STABILITY OF SILICEOUS-MAGNESITE MINERAL ASSEMBLAGE AT HYDROTHERMAL CONDITIONS.SHCHERBAN' IP; SHIROKIKH IN.1969; AKAD. NAUK S.S.S.R., SIB. OTD., GEOL. GEOFIZ ; SUN; 1969(8), NUM. 0008, P. 116 A 118Miscellaneous

DONNEES THERMODYNAMIQUES ET EXPERIMENTALES SUR LES CONDITIONS DE MANIFESTATION DE LA METASOMATOSE MAGNESIENNE DANS LES ROCHES CARBONATEES ET ALUMOSILICATEESSHCHERBAN' IP; ARKHIPENKO DK; SHIROKIKH IN et al.1971; GEOL. I GEOFIZ.; S.S.S.R.; 1971, NUM. 0007, P. 113 A 118Serial Issue

CALCUL PAR BINOMES EN COLONNES DE LA DIFFUSION ET DE L'INFILTRATION METASOMATIQUESPEN'KOVSKIJ VI; SHCHERBAN EV; SHCHERBAN IP et al.1976; DOKL. AKAD. NAUK S.S.S.R.; S.S.S.R.; 1976, VOL. 225, NUM. 0006, P. 1416 A 1419Serial Issue

PRO ZNAKHIDKU TAL'KU V ARGILIZITAKH TA PETROLOGICHNE ZNACHENNYA TS'OGO FAKTU = DISCOVERY OF TALC IN ARGILLITES AND PETROLOGICAL IMPORTANCE OF THIS FACT = LA DECOUVERTE DE TALC DANS LES ARGILITES ET L'IMPORTANCE PETROLOGIQUE DE CE FAITSHCHERBAN' IP; MOVCHAN MP; SHEVCHENKO VI et al.1981; DOPOV. AKAD. NAUK UKR. RSR, SER. B: GEOL. KHIM. BIOL. NAUKI; ISSN 0002-3523; SUN; DA. 1981; VOL. 1981; NO 5; PP. 33-35; ABS. ENG; BIBL. 1 REF.; 1 TAB. ; ILL.Article

CALCUL D'UNE DES VARIANTES DE LA DIFFUSION DANS LA ZONALITE METASOMATIQUEPEN'KOVSKIJ VI; SHCHERBAN EV; SHCHERBAN IP et al.1973; DOKL. AKAD. NAUK S.S.S.R.; S.S.S.R. ; 1973, VOL. 210, NUM. 0002, P. 452 A 455Serial Issue

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