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au.\*:("NIKITINA VN")

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LES CYANOPHYCEES DE CERTAINES SOURCES THERMALES DU CAUCASENIKITINA VN.1974; VEST. LENINGRAD. UNIV.; S.S.S.R.; DA. 1974; NO 9; PP. 56-63; ABS. ANGL.; BIBL. 1P.Article

ASSOCIATION DE CYANOPHYCEES DE QUELQUES SOURCES THERMALES DES REGIONS DE STAVROPOL ET DE KRASNODAR ET DE GEORGIENIKITINA VN.1975; VEST. LENINGRAD. UNIV.; S.S.S.R.; DA. 1975; NO 3; PP. 54-59; ABS. ANGL.; BIBL. 4REFArticle

THERMAL MODELS OF ARCS AND RIDGES - A "SOURCE-SPAN-SINK" MODEL.LUBIMOVA EA; NIKITINA VN.1978; TECTONOPHYSICS; NETHERL.; DA. 1978; VOL. 45; NO 4; PP. 341-362; BIBL. 1 P. 1/2; 11 ILL.Article

ON HEAT FLOW SINGULARITIES OVER MID-OCEAN RIDGES.LUBIMOVA EA; NIKITINA VN.1975; J. GEOPHYS. RES.; U.S.A.; DA. 1975; VOL. 80; NO 2; PP. 232-243; BIBL. 17 REF.Article

DETERMINATION OF THE ELECTRIC PROPERTIES OF ROCK IN ITS NATURAL STATE IN THE CRYSTALLINE BASEMENT.NIKITINA VN; ENENSHTEJN BS.1968; IZVEST. ACAD. SCI. U.S.S.R., PHYS. SOLID EARTH; USA; 1968(12), NUM. 0012, P. 748 A 753Miscellaneous

SOLUTION DU PROBLEME AUX LIMITES DES CHAMPS THERMIQUES ET ELECTROMAGNETIQUES DE LA TERRE AU-DESSUS DU CONTACT VERTICAL DE MILIEUX DE STRATIFICATION HORIZONTALELYUBIMOVA EA; NIKITINA VN.1975; IN: ISSLED. TEPL. EHLEKTROMAGN. POLEJ SSSR; MOSKVA; NAUKA; DA. 1975; PP. 5-19; ABS. ANGL.; BIBL. 3 REF.Book Chapter

UNE FORME THERMOPHILE INHABITUELLE DE MASTIGOCLADUS LAMINOSUSNIKITINA VN; GERASIMENKO LM.1983; MIKROBIOLOGIJA (MOSKVA); ISSN 50727X; SUN; DA. 1983; VOL. 52; NO 3; PP. 477-481; ABS. ENG; BIBL. 5 REF.Article

ETUDE DES CARACTERISTIQUES FREQUENTIELLES DYNAMIQUES DES STRUCTURES GEOELECTRIQUES STRATIFIEES.IVANOV AP; NIKITINA VN.1968; IZVEST. AKAD. NAUK S.S.S.R., FIZ. ZEMLI; SUN; 1968(3), NUM. 0003, P. 55 A 62Miscellaneous

INVESTIGATION OF THE DYNAMIC FREQUENCY CHARACTERISTICS OF LAYERED GEOELECTRIC STRUCTURES.IVANOV AP; NIKITINA VN.1968; IZVEST. ACAD. SCI. U.S.S.R., PHYS. SOLID EARTH; USA; 1968(3), NUM. 0003, P. 174 A 177Miscellaneous

ETUDE DE LA STRUCTURE DE LA CROUTE TERRESTRE PAR LA METHODE DE SONDAGE ELECTROMAGNETIQUE FREQUENTIELNIKITINA VN; EHNENSHTEJN BS.1977; IZVEST. AKAD. NAUK S.S.S.R., FIZ. ZEMLI; S.S.S.R.; DA. 1977; NO 1; PP. 90-100; BIBL. 1 P. 1/2Article

SUMMARY THERMAL MODEL FOR ISLAND ARCS AND RIDGES.LUBIMOVA EA; NIKITINA VN; VOLKOVA NA et al.sdIN: INT. UNION GEOD. GEOPHYS. GEN. ASSEM. 16; GRENOBLE; 1975; PARIS IMPR. SCHIFFER; RESUME,1975, P. 90Miscellaneous

ANALYSIS OF THE HEAT-FLUX SINGULARITY ABOVE MID-OCEAN RIDGES.LYUBIMOVA YE A; LYUBIMOVA EA; NIKITINA VN et al.sdDOKL. EARTH SCI. SECT.; U.S.A.; DU RUSSE: DOKL. AKAD. NAUK S.S.S.R., S.S.S.R. 1974; 216, NO 3, 540-543,1975, VOL. 216, P. 13 A 15Miscellaneous

A STUDY OF INTRINSIC STRUCTURE OF THE CRYSTALLINE BASEMENT BY ELECTROMAGNETIC PROBING.TIKHONOV AN; ENENSHTEJN BS; SKUGAREVSKAJA OA et al.1967; DOKL. EARTH SCI. SECT.; USA; 1967(4), VOL. 173, P. 4 A 6Miscellaneous

MODELE THERMIQUE DES ZONES DE RIFT CONTINENTAUX ET OCEANIQUES SUR L'EXEMPLE DE LA MER ROUGE ET DU LAC BAIKALLYUBIMOVA EA; NIKITINA VN; KOPERBAKH EB et al.1978; DOKL. AKAD NAUK S.S.S.R.; SUN; DA. 1978; VOL. 243; NO 1; PP. 62-65; BIBL. 14 REF.Article

TEPLOVYE POLYA VNUTRENNIKH I OKRAINNYKH MOREJ SSSR. SOSTOYANIE NABLYUDENIJ I TEORIYA INTERPRETATSII DVUMERNYKH NEODNORODNOSTEJ. = CHAMPS THERMIQUES DES MERS INTERNES ET EPICONTINENTALES DE L'URSS. ETATS DES OBSERVATIONS ET THEORIE DE L'INTERPRETATION DES HETEROGENEITES A DEUX DIMENSIONSLYUBIMOVA EA; NIKITINA VN; TOMARA GA et al.1976; MOSKVA; NAUKA; DA. 1976; PP. 1-222; H.T. 1; BIBL. 5 P.; 55 ILL.Book

GLUBINA ASTENOSFERICHESKOGO SLOYA NA OSNOVE ZNACHENIJ GEOMETRICHESKIKH I GEOHLEKTRICHESKIKH MODELEJ = PROFONDEUR DE L'ASTHENOSPHERE D'APRES LES VALEURS DE MODELES GEOMETRIQUES ET GEOELECTRIQUESLYUBIMOWA EA; LYUBIMOVA EA; NIKITINA WN et al.1980; GEODAET. GEOPHYS. VEROEFF., AKAD. WISS. DDR; DDR; DA. 1980; VOL. 3; NO 47; PP. 113-124; BIBL. 36 REF.; ILL.Conference Paper

CONTINENTAL MARGIN THERMAL MODEL FOR KURIL ISLAND ARC AND SEA OF OKHOTSKSAMARSKY AA; LUBIMOVA EA; NIKITINA VN et al.1977; GEOPHYS. RES. BULL.; IND; DA. 1977; VOL. 15; NO 4; PP. 111-122; BIBL. 14 REF.Article

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