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A HIGH-EFFICIENCY CARBAZINE-122 DYE LASER.KOTO K.1976; OPT. COMMUNIC.; NETHERL.; DA. 1976; VOL. 18; NO 4; PP. 447-448; BIBL. 6 REF.Article

OUTLOOK ON CITY GAS INDUSTRIESKOTO K; KUSANO S.1980; NENRYO KYOKAI-SHI; ISSN 0369-3775; JPN; DA. 1980; VOL. 59; NO 11; PP. 885-895; ABS. ENG; BIBL. 8 REF.Article

PHOSPHODIESTERASES OF TOBACCO CELL CULTURES AND THE INTACT PLANT.SHINSHI H; KOTO K.1977; PHYTOCHEMISTRY; G.B.; DA. 1977; VOL. 16; NO 11; PP. 1661-1662; BIBL. 7 REF.Article

PHASE RELATIONS OF THE CU-S SYSTEM AT LOW TEMPERATURES : STABILITY OF ANILITE.MORIMOTO N; KOTO K.1970; AMER.MINERALOGIST.; 1970, VOL. 55, P. 106 A 117Miscellaneous

DISORDER OF METAL ATOMS IN THE STRUCTURE OF QUENCHED HIGH-TEMPERATURE CUBANITE, CUFE2S3, Z=4/3 = DESORDRE DES ATOMES METALLIQUES DANS LA STRUCTURE DE LA CUBANITE DE HAUTE TEMPERATURE TREMPEE, CUFE2S3, Z=4/3MIZOTA T; KOTO K.1983; MINERALOGICAL JOURNAL; ISSN 0544-2540; JPN; DA. 1983; VOL. 11; NO 5; PP. 213-221; BIBL. 19 REF.; TABL./ILL.Article

Wasserstoff statt Erdgas in der Energieversorgung? = Hydrogen instead of natural gas in the energy supply?KOTO, K.Gas- und Wasserfach. Gas - Erdgas. 1992, Vol 133, Num 7, pp 332-335, issn 0016-4909Article

En Japonais = EXAFS and its application in mineralogyKOTO, K.Kobutsugaku Zasshi. 1990, Vol 19, Num 6, pp 357-360, issn 0454-1146Article

THE SUPERSTRUCTURE OF THE INTERMEDIATE PYRRHOTITE. II: ONE-DIMENSIONAL OUT-OF-STEP VECTOR OF FE VACANCIES IN THE INCOMMENSURATE STRUCTURE WITH COMPOSITIONAL RANGE FROM FE9S10 TO FE11S12 = SURSTRUCTURE DE LA PYRRHOTITE INTERMEDIAIRE. II: VECTEUR UNIDIMENSIONNEL ANORMAL DES LACUNES DE FER DANS LA STRUCTURE DISPROPORTIONNEE POUR UNE COMPOSITION ALLANT DE FE9S10 A FE11S12KOTO K; KITAMURA M.1981; ACTA CRYSTALLOGR., SECT. A, CRYST. PHYS., DIFFR., THEOR. GEN. CRYSTALLOGR.; ISSN 0567-7394; DNK; DA. 1981; VOL. 37; NO 3; PP. 301-308; BIBL. 10 REF.; ILL.Article

Use of hydrogen in town gas systemsKOTO, K.Gas, Wärme international. 1991, Vol 40, Num 12, pp 525-528, issn 0020-9384Article

Minéraux à structure tunnel. IntroductionKOTO, K.Kobutsugaku Zasshi. 1985, Vol 16, Num 6, pp 435-436, issn 0454-1146Article

THE SUPERSTRUCTURE OF THE INTERMEDIATE PYRRHOTITE. II: ONE-DIMENSIONAL OUT-OF-STEP VECTOR OF FE VACANCIES IN THE INCOMMENSURATE STRUCTURE WITH COMPOSITIONAL RANGE FROM FE9S10 TO FE11S12 = SURSTRUCTURE DE LA PYRRHOTITE INTERMEDIAIRE. II: VECTEUR UNIDIMENSIONNEL ANORMAL DES LACUNES DE FER DANS LA STRUCTURE DISPROPORTIONNEE POUR UNE COMPOSITION ALLANT DE FE9S10 A FE11S12KOTO K; KITAMURA M.1981; ACTA CRYSTALLOGR., SECT. A, CRYST. PHYS., DIFFR., THEOR. GEN. CRYSTALLOGR.; ISSN 0567-7394; DNK; DA. 1981; VOL. 37; NO 3; PP. 301-308; BIBL. 10 REF.Article

X-RAY DIFFUSE SCATTERING FROM WURTZITE-TYPE COMPOUNDSKOTO K; SCHULZ H.1979; ACTA CRYSTALLOGR., SECT. A, CRYST. PHYS. DIFFR., THEOR. GEN. CRYSTALLOGR.; DNK; DA. 1979; VOL. 35; NO 6; PP. 971-974; BIBL. 7 REF.Article

A SYSTEMATICS OF PYROXENOID STRUCTURES.TAKEUCHI Y; KOTO K.1977; MINERAL. J.; JAP.; DA. 1977; VOL. 8; NO 5; PP. 272-285; BIBL. 23 REF.; 9 ILL.Article

SUPERSTRUCTURE INVESTIGATION OF BORNITE, CU5FES4, BY THE MODIFIED PARTITIAL PATTERSON FUNCTION.KOTO K MORIMOTO N.1975; ACTA CRYSTALLOGR., B; DANEM.; DA. 1975; VOL. 31; NO 9; PP. 2268-2273; BIBL. 17 REF.; 8 ILL.Article

CRYSTALLOGRAPHIC RELATIONSHIPS OF THE PYROXENES AND PYROXENOIDS.KOTO K; MORIMOTO N; NARITA H et al.1976; J. JAP. ASS. MINERALOGISTS PETROLOGISTS ECON. GEOLOGISTS; JAP.; DA. 1976; VOL. 71; NO 8; PP. 248-254; ABS. JAP.; BIBL. 15 REF.; 5 ILL.Article

ANILITE, CU7S4, A NEW MINERAL.MORIMOTO N; KOTO K; SHIMAZAKI Y et al.1969; AMER.MINERALOGIST.; 1969(10), VOL. 54, P. 1256 A 1268Miscellaneous

BORNITE (CU5FES4): STABILITY AND CRYSTAL STRUCTURE OF THE INTERMEDIATE FORMKANAZAWA Y; KOTO K; MORIMOTO N et al.1978; CANAD. MINERALOGIST; CAN; DA. 1978; VOL. 16; NO 3; PP. 397-404; ABS. FRE; BIBL. 14 REF.; 5 ILL.Article

ANION DISORDER AND IONIC MOTION IN LEAD FLUORIDE (BETA -PBF2)KOTO K; SCHULZ H; HUGGINS RA et al.1980; SOLID STATE IONICS; NLD; DA. 1980; VOL. 1; NO 5-6; PP. 355-365; BIBL. 31 REF.Article

THE CRYSTAL STRUCTURES OF MNSIO3 POLYMORPHS (RHODONITE- AND PYROXMANGITE-TYPE).NARITA H; KOTO K; MORIMOTO N et al.1977; MINERAL. J.; JAP.; DA. 1977; VOL. 8; NO 6; PP. 329-342; BIBL. 1 P.Article

UEBER PEARCEIT, POLYBASIT UND BINNIT. (PEARCEITE, POLYBASITE ET TETRAEDRITE).EDENHARTER A; KOTO K; NOWACKI W et al.1971; NEU. JB. MINERAL., MONATSCH.; DEU; 1971(8), VOL. 1971, NUM. 0008, P. 337 A 341Miscellaneous

Superstructures and phase transitions of Bi2O3TSUBAKI, M; KOTO, K.Materials research bulletin. 1984, Vol 19, Num 12, pp 1613-1620, issn 0025-5408Article

LITHIUM-HYDRORHODONITE.MURAKAMI T; TAKEUCHI Y; TAGAI T et al.1977; ACTA CRYSTALLOGR., B; DANEM.; DA. 1977; VOL. 33; NO 3; PP. 919-921; BIBL. 9 REF.; 2 ILL.Article

THE CRYSTAL STRUCTURE OF NAMBULITE (LI,NA)MN4SI5O14 (OH).NARITA H; KOTO K; MORIMOTO N et al.1975; ACTA CRYSTALLOGR., B; DANEM.; DA. 1975; VOL. 31; NO 10; PP. 2422-2426; BIBL. 14 REF.; 2 ILL.Article

THE CRYSTAL STRUCTURE OF SARABANITE CASB10O10S6, A NEW OXIDE SULFIDE MINERAL.NAKAI I; KOTO K; NAGASHIMA K et al.1977; CHEM. LETTERS; JAP.; DA. 1977; NO 3; PP. 275-276; BIBL. 3 REF.Article

SUPERSTRUCTURE AND NONSTOICHIOMETRY OF INTERMEDIATE PYRRHOTITE.MORIMOTO N; GYOBU A; TSUKUMA K et al.1975; AMER. MINERALOGIST; U.S.A.; DA. 1975; VOL. 60; NO 3-4; PP. 240-248; BIBL. 1 P.; 10 ILL.Article

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