FORMATION OF OLIVINE TEXTURES IN PALLASITES AND THERMAL HISTORY OF PALLASITES IN THEIR PARENT BODY = FORMATION DES TEXTURES DE L'OLIVINE DANS LES PALLASITES ET HISTOIRE THERMIQUE DES PALLASITES DANS LEUR CORPS D'ORIGINEOHTANI E.1983; PHYSICS OF THE EARTH AND PLANETARY INTERIORS; ISSN 0031-9201; NLD; DA. 1983; VOL. 32; NO 2; PP. 182-192; BIBL. 29 REF.Article

MELTING RELATION OF FE₂SIO₄ UP TO ABOUT 200 KBAROHTANI E.1979; J. PHYS. EARTH; JPN; DA. 1979; VOL. 27; NO 3; PP. 189-208; BIBL. 2 P.Article

Fractionation process and consitution of the Earth's interiorOHTANI, E.Kobutsugaku Zasshi. 1991, Vol 20, Num 4, pp 209-216, issn 0454-1146Article

The primodial terrestrial magma ocean and its implication for stratification of the mantle = Océan de magma terrestre primitif et implication sur la stratification du manteauOHTANI, E.Physics of the earth and planetary interiors. 1985, Vol 38, Num 1, pp 70-80, issn 0031-9201Article

Generation of komatiite magma and gravitational differentiation in the deep upper mantle = Génération de magma komatiite et différenciation par gravité dans le manteau supérieur profondOHTANI, E.Earth and planetary science letters. 1984, Vol 67, Num 2, pp 261-272, issn 0012-821XArticle

MELTING OF FORSTERITE MG₂SIO₄ UP TO 15 GPA = FUSION DE LA FORSTERITE JUSQU'A 15 GPAOHTANI E; KUMAZAWA M.1981; PHYS. EARTH PLANET. INTER.; ISSN 0031-9201; NLD; DA. 1981; VOL. 27; NO 1; PP. 32-38; BIBL. 16 REF.; ILL./TABL.Article

Study of minerals as functions of temperature, pressure, and compositionOHTANI, E.Kobutsugaku Zasshi. 1992, Vol 21, Num 4, pp 233-237, issn 0454-1146Article

Ultrahigh pressure melting and chemical heterogeneity in the deep mantleOHTANI, E.Dynamic processes of material transport and transformation in the Earth's interior. 1990, pp 309-325Book Chapter

Melting temperature distribution and fractionation in the lower mantle = Distribution de la température de fusion et fractionnement dans le manteau inférieurOHTANI, E.Physics of the earth and planetary interiors. 1983, Vol 33, Num 1, pp 12-25, issn 0031-9201Article

PHASE RELATIONS IN THE SYSTEMS FE₂SIO₄-FEAL₂O₄ AND CO₂SIO₄-COAL₂O₄ AT HIGH PRESSURE AND HIGH TEMPERATURE.OHTANI E; SAWAMOTO H.1976; MINERAL. J.; JAP.; DA. 1976; VOL. 8; NO 4; PP. 226-233; BIBL. 11 REF.; 1 ILL.Article

Majorite fractionation and genesis of komatiites in the deep mantle = Fractionnement de Majorite et genèse de komatïtes dans les zones profondes du manteauOHTANI, E.Precambrian research. 1990, Vol 48, Num 3, pp 195-202, issn 0301-9268, 8 p.Conference Paper

Chemical stratification of the mantle formed by melting in the early stage of the terrestrial evolution = Stratification chimique du manteau formée par fusion pendant les premières étapes de l'évolution terrestreOHTANI, E.Tectonophysics. 1988, Vol 154, Num 3-4, pp 201-210, issn 0040-1951Article

STABILITY FIELD OF KNORRINGITE MG₃CR₂SI₃O₁₂ AT HIGH PRESSURE AND ITS IMPLICATION TO THE OCCURRENCE OF CR-RICH PYROPE IN THE UPPER MANTLE = DOMAINE DE STABILITE DE LA KNORRINGITE A HAUTE PRESSION ET IMPLICATION CONCERNANT L'OCCURRENCE DE PYROPE RICHE EN CHROME DANS LE MANTEAU SUPERIEURIRIFUNE T; OHTANI E; KUMAZAWA M et al.1982; PHYS. EARTH PLANET. INTER.; ISSN 0031-9201; NLD; DA. 1982; VOL. 27; NO 4; PP. 263-272; BIBL. 29 REF.Article

THERMAL EXPANSION OF MODIFIED SPINEL, BETA -MG₂SIO₄ = EXPANSION THERMIQUE DU SPINELLE MODIFIE BETA -MG₂SIO₄SUZUKI I; OHTANI E; KUMAZAWA M et al.1980; J. PHYS. EARTH; ISSN 0022-3743; JPN; DA. 1980; VOL. 28; NO 3; PP. 273-280; BIBL. 17 REF.; 3 TAB. ; TABL./ILL.Article

HIGH PRESSURE DECOMPOSITION OF GAMMA -FE₂SIO₄.SAWAMOTO H; OHTANI E; KUMAZAWA M et al.1975; IN: COLLECT. PAP. EARTH SCI., 1974; NAGOYA; NAGOYA UNIV.; DA. 1975; PP. 194-201; BIBL. 23 REF.; 12 ILL.; TIRE A PART DE: PROC. 4TH INT. CONF. HIGH PRESS.; KYOTO; 1974Book Chapter

EFFECT OF BETA -SUBSTITUENTS ON THE CONFIGURATIONAL STABILITY OF ALPHA -FLUOROCYCLOPROPYL RADICALSISHIHARA T; OHTANI E; ANDO T et al.1975; J. CHEM. SOC., CHEM. COMMUNIC.; G.B.; DA. 1975; NO 9; PP. 367-368; BIBL. 4 REF.Article

FUSION OF PYROPE AT HIGH PRESSURES AND RAPID CRYSTAL GROWTH FROM THE PYROPE MELT = FUSION DU PYROPE A HAUTES PRESSIONS ET CROISSANCE CRISTALLINE RAPIDE A PARTIR DU PYROPE FONDUOHTANI E; IRIFUNE T; FUJINO K et al.1981; NATURE (LOND.); ISSN 0028-0836; GBR; DA. 1981; VOL. 294; NO 5836; PP. 62-64; BIBL. 9 REF.; TABL./ILL.Article

THERMAL EXPANSION OF GAMMA -MG₂SIO₄SUZUKI I; OHTANI E; KUMAZAWA M et al.1979; J. PHYS. EARTH; JPN; DA. 1979; VOL. 27; NO 1; PP. 53-61; BIBL. 18 REF.Article

GLUCOSE-PHOSPHORYLATING ENZYMES OF CANDIDA YEASTS AND THEIR REGULATION IN VIVO.HIRAI M; OHTANI E; TANAKA A et al.1976; BIOCHIM. BIOPHYS. ACTA; PAYS-BAS; DA. 1976; VOL. 480; NO 2; PP. 357-366; BIBL. 16 REF.Article

POSTPINEL PHASE OF FORSTERITE AND EVOLUTION OF THE EARTH'S MANTLE.KUMAZAWA M; SAWAMOTO H; OHTANI E et al.1974; NATURE; G.B.; DA. 1974; VOL. 247; NO 5440; PP. 356-358; BIBL. 27 REF.Article

MELTING OF VARIOUS SILICATES AT ELEVATED PRESSURES = FUSION DE SILICATES VARIES SOUS PRESSIONS ELEVEESOHTANI E; KUMAZAWA M; KATO T et al.1982; ADVANCES IN EARTH AND PLANETARY SCIENCES; ISSN 504696; JPN; DA. 1982; VOL. 12; PP. 259-270; BIBL. 1 P.Article

DECOMPOSITION OF SPINEL MGAL₂O₄ AT EXTREMELY HIGH PRESSURE.OHTANI E; SAWAMOTO H; MASAKI K et al.1975; IN: COLLECT. PAP. EARTH SCI., 1974; NAGOYA; NAGOYA UNIV.; DA. 1975; PP. 185-189; BIBL. 20 REF.; 7 ILL.; TIRE A PART DE: PROC. 4TH INT. CONF. HIGH PRESS.; KYOTO; 1974Book Chapter

REDUCTION OF 1-SUBSTITUTED 7-CHLORO-7-FLUORONORCARANES WITH TRIBUTYLTIN HYDRIDEANDO T; ISHIHARA T; OHTANI E et al.1981; J. ORG. CHEM.; ISSN 0022-3263; USA; DA. 1981; VOL. 46; NO 22; PP. 4446-4450; BIBL. 17 REF.Article

HIGH PRESSURE GENERATION BY MASS 318-90 TYPE APPARATUS.MASAKI K; SAWAMOTO H; OHTANI E et al.1975; REV. SCI. INSTRUM.; U.S.A.; DA. 1975; VOL. 46; NO 1; PP. 84-88; BIBL. 14 REF.Article

Composition of the core. I: Solubility of oxygen in molten iron at high temperatures = Composition du noyau. I: solubilité de l'oxygène dans le fer en fusion à hautes températuresOHTANI, E; RINGWOOD, A. E.Earth and planetary science letters. 1984, Vol 71, Num 1, pp 85-93, issn 0012-821XArticle