ON THE SPACE GROUP OF SPINEL, MGAL₂O₄TOKONAMI M; HORIUCHI H.1980; ACTA CRYSTALLOGR., SECT. A, CRYST. PHYS., DIFFR., THEOR. GEN. CRYSTALLOGR.; ISSN 0567-7394; DNK; DA. 1980; VOL. 36; NO 1; PP. 122-126; BIBL. 7 REF.Article

DOMAIN STRUCTURE OF PIGEONITE AND CLINOENSTATITE.MORIMOTO N; TOKONAMI M.1969; AMER.MINERALOGIST.; 1969(6), VOL. 54, P. 725 A 740Miscellaneous

ORIENTED EXSOLUTION OF AUGITE IN PIGEONITE.MORIMOTO N; TOKONAMI M.1969; AMER.MINERALOGIST.; 1969(8), VOL. 54, P. 1101 A 1117Miscellaneous

A STUDY OF SUBSOLIDUS RELATIONS OF THE SKAERGAARD PYROXENES BY ANALYTICAL ELECTRON MICROSCOPYNOBUGAI K; TOKONAMI M; MORIMOTO N et al.1978; CONTRIB. MINERAL. PETROL.; DEU; DA. 1978; VOL. 67; NO 2; PP. 111-117; BIBL. 16 REF.; 6 ILL.Article

CRYSTAL FIELD EFFECT ON THE OLIVINE SPINEL TRANSFORMATION.SYONO Y; TOKONAMI M; MATSUI Y et al.1971; PHYS. EARTH PLANET. INTER.; NLD; 1971, VOL. 4, NUM. 0005, P. 347 A 352Miscellaneous

MAJOR ELEMENT COMPOSITION OF CLAY MINERALS IN THE MURCHISON (C2) CARBONACEOUS CHONDRITE MATRIX = ELEMENTS MAJEURS DES MINERAUX ARGILEUX DANS LA MATRICE DE LA CHONDRITE CARBONEE MURCHISON (C2)NORO H; NAGASAWA K; TOKONAMI M et al.1980; MEM. NATL. INST. POLAR RES., SPEC. ISSUE; ISSN 0386-0744; JPN; DA. 1980; NO 17; PP. 311-317; BIBL. 7 REF.Conference Paper

TWIN FORMATION BY A COMPRESSIVE STRESS ON THE TRANSITION OF CSCLWATANABE M; TOKONAMI M; MORIMOTO N et al.1980; J. SOLID STATE CHEM.; GBR; DA. 1980; VOL. 31; NO 2; PP. 265-268; BIBL. 7 REF.Article

CRYSTAL STRUCTURES OF V_NO_2N-1(2 <OU= N <OU= 7).HORIUCHI H; MORIMOTO N; TOKONAMI M et al.1976; J. SOLID STATE CHEM.; G.B.; DA. 1976; VOL. 17; NO 4; PP. 407-424; BIBL. 26 REF.Article

DISTRIBUTION OF TITANIUM ATOMS IN OXY-KAERSUTITE.KITAMURA M; TOKONAMI M; MORIMOTO N et al.1975; CONTRIB. MINERAL. PETROL.; GERM.; DA. 1975; VOL. 51; NO 3; PP. 167-172; BIBL. 11 REF.Article

REFINEMENT OF 3C PYRRHOTITE, FE₇S₈NAKANO A; TOKONAMI M; MORI MOTO N et al.1979; ACTA CRYSTALLOGR., B; DNK; DA. 1979; VOL. 35; NO 3; PP. 722-724; BIBL. 10 REF.Article

DISTRIBUTION OF TITANIUM ATOMS IN OXY-KAERSUTITE.KITAMURA M; TOKONAMI M; MORIMOTO N et al.1975; CONTRIB. MINERAL. PETROL.; GERM.; 1975, VOL. 51, NUM. 0003, P. 167 A 172Serial Issue

THE CRYSTAL STRUCTURE OF OMPHACITE.MATSUMOTO T; TOKONAMI M; MORIMOTO N et al.1975; AMER. MINERALOGIST; U.S.A.; DA. 1975; VOL. 60; NO 7-8; PP. 634-641; BIBL. 1 P.; 2 ILL.Article

CRYSTAL CHEMISTRY OF MNGEO₃ POLYMORPHS = CRISTALLOCHIMIE DES POLYMORPHES MNGEO₃MIRANO M; TOKONAMI M; MORIMOTO N et al.1980; KOBUTSUGAKU ZASSHI; ISSN 0454-1146; JPN; DA. 1980; VOL. 14; NO SPEC 3; PP. 158-164; ABS. ENG; BIBL. 11 REF.Article

THE DIFFRACTION ASPECT AND A STRUCTURAL MODEL OF MULLITE, AL(AL_1+2XSI_1-2X)O_5-XTOKONAMI M; NAKAJIMA Y; MORIMOTO N et al.1980; ACTA CRYSTALLOGR. SECT. A, CRYST. PHYS., DIFFR., THEOR. GEN. CRYSTALLOGR.; ISSN 0567-7394; DNK; DA. 1980; VOL. 36; NO 2; PP. 270-276; BIBL. 12 REF.Article

The anharmonic thermal vibration in ZnX (X=S, Se, Te) and its dependence on the chemical-bond charactersYAMANAKA, T; TOKONAMI, M.Acta crystallographica. Section B, Structural science. 1985, Vol 41, Num 5, pp 298-304, issn 0108-7681Article

Laser-induced changes in the electron density distribution of crystals : Ca₃Cr₂Si₃O₁₂SAWADA, H; TOKONAMI, M.Zeitschrift für Physik. B, Condensed matter. 1992, Vol 87, Num 2, pp 163-164, issn 0722-3277Article

Diffusion of rare-earth elements in fish teeth from deep-sea sediments = Diffusion des terres rares dans les dents de poissons des sédiments de mer profondeTOYODA, Z; TOKONAMI, M.Nature (London). 1990, Vol 345, Num 6276, pp 607-609, issn 0028-0836, 3 p.Article

STABILITY RELATIONS BETWEEN OLIVINE, SPINEL AND MODIFIED SPINEL.TOKONAMI M; MORIMOTO N; AKIMOTO S et al.1972; EARTH PLANET. SCI. LETTERS; NLD; 1972, VOL. 14, NUM. 0001, P. 65 A 69Miscellaneous

CRYSTAL STRUCTURES OF HIGH PRESSURE MODIFICATIONS OF MN2GEO4 AND CO2SIO4.MORIMOTO N; AKIMOTO S; KOTO K et al.1970; PHYS. EARTH PLANET. INTER.; NLD; 1970, VOL. 3, P. 161 A 165Miscellaneous

THE EXISTENCE OF PARTIAL MIRRORS IN WOLLASTONITE.ITO T; SADANAGA R; TAKEUCHI Y et al.1969; PROC. JAP. ACAD.; JPN; 1969, VOL. 45, NUM. 0010, P. 913 A 918Miscellaneous

Crystal structure and cation distribution of «cleavable» olivines = Structure cristalline et répartition des cations des olivines «clivables»AIKAWA, N; TOKONAMI, M.Mineralogical Journal. 1987, Vol 13, Num 5, pp 271-279, issn 0544-2540Article

Coexisting sodic augite and omphacite in a Sanbagawa metamorphic rock, Japan = Coexistence de l'augite sodique et de l'omphacite dans une roche métamorphique de Sanbagawa ― JaponENAMI, M; TOKONAMI, M.Contributions to mineralogy and petrology. 1984, Vol 86, Num 3, pp 241-247, issn 0010-7999Article

THE CRYSTAL STRUCTURE OF THE PYROXENE-TYPE MNSIO₃ = STRUCTURE CRISTALLINE DE MNSIO₃ TYPE PYROXENETOKONAMI M; HORIUCHI H; NAKANO A et al.1979; MINERALOGICAL JOURNAL; ISSN 0544-2540; JPN; DA. 1979; VOL. 9; NO 7; PP. 424-426; BIBL. 6 REF.; TABL.Article

CRYSTAL STRUCTURES OF HIGH PRESSURE MODIFICATIONS OF MN2GEO4 AND CO2SIO4.MORIMOTO N; AKIMOTO S; KOTO K et al.1970; PHYS. EARTH PLANET. INTER.; NLD; 1970, VOL. 3, P. 161 A 165Miscellaneous

PYRRHOTITES : STOICHIOMETRIC COMPOUNDS WITH COMPOSITION FEN-1SN (N =- OR = 8).MORIMOTO N; NAKAZAWA H; NISHIGUCHI K et al.1970; SCIENCE; USA; 1970(5), VOL. 168, NUM. 3934, P. 964 A 966Miscellaneous