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GEDANKEN ZUM STABILEN PHASENDIAGRAMM DER PLAGIOKLASE = REFLEXIONS SUR LE DIAGRAMME D'EQUILIBRE STABLE DU PLAGIOCLASELAVES F.1979; SCHWEIZ. MINERAL. PETROGR. MITT.; CHE; DA. 1979; VOL. 59; NO 1-2; PP. 19-23Article

DIE MINERALOGISCH-PETROGRAPHISCHE SAMMLUNG. (LA COLLECTION MINERALOGICO-PETROGRAPHIQUE).LAVES F.1970; VIERTELJ.-SCHR. NATURFORSCH. GESELLSCH. ZUERICH; CHE; 1970(12), VOL. 115, NUM. 0004, P. 461 A 462Miscellaneous

GEDANKEN ZUM STABILEN PHASENDIAGRAMM DER PLAGIOKLASE = IDEES SUR LE DIAGRAMME DE PHASES STABLES DES PLAGIOCLASESLAVES F.1977; DIE HOHEN TAUERN - MINERALOGIE U. PETROLOGIE; AUT; SALZBURG: OESTERR. MINERAL. GES.; DA. 1977; PP. 15; ILL.Book Chapter

DIE THERMOLUMINESZENZ VON QUARZEN (BERGKRISTALL, RAUCHQUARZ UND DERBES MATERIAL) AUS DEN SCHWEIZER ALPEN. = LA THERMOLUMINESCENCE DES QUARTZS (CRISTAL DE ROCHE, QUARTZ FUME ET MATERIAUX BRUTS DES ALPES SUISSESBAECHTIGER K; LAVES F.sdFORTSCH. D. MINERAL., BEIH.; DTSCH.; (53. JAHRESTAG. DEUTSCHEN MINERAL. GES.; HEIDELBERG; 1975),1975, VOL. 53, NUM. 0001, P. 2Miscellaneous

HOW MANY FACES HAS THE LARGEST SPACE-FILLING POLYHEDRON.BRUNNER GO; LAVES F.1978; Z. KRISTALLOGR.; DDR; DA. 1978; VOL. 147; NO 1-2; PP. 39-43; ABS. GER; BIBL. 15 REF.Article

THE MUTUAL ORIENTATION OF PERISTERITE PHASES.LAVES F; WEBER L.1971; NATURWISSENSCHAFTEN; 1971, VOL. 361, NUM. 0007Miscellaneous

SYNTHESIS AND X-RAY REFLECTION PATTERN OF BETA-EUCRYPTITE.TSCHERRY V; LAVES F.1970; NATURWISSENSCH.-DTSCH.; 1970(4), VOL. 57, NUM. 0004Miscellaneous

AVERAGE AND SUPER STRUCTURE OF BETA EUCRYPTITE (LIALSIO4). I. AVERAGE STRUCTURETSCHERRY V; SCHULZ H; LAVES F et al.1972; Z. KRISTALLOGR.; DTSCH.; 1972, VOL. 135, NUM. 0003-0004, P. 161 A 174Serial Issue

TEMPERATURABHAENGIGKEIT DER GITTERKONSTANTEN UND DER REFLEX-INTENSITAETEN VON ANORTHIT. (CONSTANTES DE RESEAU ET POUVOIR REFLECTEUR DE L'ANORTHITE EN FONCTION DE LA TEMPERATURE).CZANK M; LAVES F; SCHULZ H et al.1970; FORTSCHR. D. MINERAL.; DEU; 1970(5), VOL. 47, NUM. 0001Miscellaneous

AVERAGE AND SUPER STRUCTURE OF BETA EUCRYPTITE (LIALSIO4). II. SUPERSTRUCTURETSCHERRY V; SCHULZ H; LAVES F et al.1972; Z. KRISTALLOGR.; DTSCH.; 1972, VOL. 135, NUM. 0003-0004, P. 175 A 198Serial Issue

SYNTHESE UND EINKRISTALLUNTERSUCHUNGEN VON HOCH-EUKRYPTIT, BETA-LI AL SIO4. (SYNTHESE ET ETUDES D'UN CRISTAL D'EUKRYPTITE, BETA-LI AL SIOTSCHERRY V; SCHULZ H; LAVES F et al.1970; FORTSCHR. D. MINERAL.; DEU; 1970(5), VOL. 47, NUM. 0001Miscellaneous

LIGHT SCATTERING OF HEAT-TREATED QUARTZ IN RELATION TO HYDROGEN-CONTAINING DEFECTS.BAMBAUER HU; BRUNNER GO; LAVES F et al.1969; AMER.MINERALOGIST.; 1969(6), VOL. 54, P. 718 A 724Miscellaneous

NUCLEAR MAGNETIC RESONANCE OF 23NA, 27AL, AND 29SI AND CATION DISORDER IN NEPHELINEBRINKMANN D; GHOSE S; LAVES F et al.1972; Z. KRISTALLOGR.; DTSCH.; 1972, VOL. 135, NUM. 0003-0004, P. 208 A 218Serial Issue

ON THE DOMAINS OF ANORTHITE.CZANK M; LAVES F; SCHULZ H et al.1970; NATURWISSENSCH.-DTSCH.; 1970(3), VOL. 57, NUM. 0003Miscellaneous

DIE REGIONALE VERTEILUNG DER THERMOLUMINESZENZ VON QUARZEN (BERGKRISTALL, RAUCHQUARZ UND DERBES MATERIAL) AUS DEN SCHWEIZER ALPEN. = REPARTITION REGIONALE DE LA THERMOLUMINESCENCE DE QUARTZ (CRISTAL DE ROCHE, QUARTZ FUME, MATIERE DURE) DES ALPES SUISSESBACHTIGER K; BRUNNER GO; LAVES F et al.1975; SCHWEIZ. MINERAL. PETROGR. MITT.; SCHWEIZ; DA. 1975; VOL. 55; NO 3; PP. 586-588; BIBL. 14 REF.; (HAUPTVERSAMML. SCHWEIZ. MINERAL. PETROGR. GES. SO. BER.; AARAU; 1975)Conference Paper

THE TEMPERATURE DEPENDENCE OF THE REFLECTION INTENSITIES OF ANORTHITE (CAAL2SI2O8) AND THE CORRESPONDING FORMATION OF DOMAINS.LAVES F; CZANK M; SCHULZ H et al.1970; SCHWEIZ. MINERAL. PETROGR. MITT.; CHE; 1970, VOL. 50, NUM. 0003, P. 519 A 525Miscellaneous

SYNTHESE UND EINKRISTALLUNTERSUCHUNGEN VON HOCH-EUKRYPTIT, BETA -LIALSIO4 (RESUME).TSCHERRY V; SCHULZ H; LAVES F et al.1969; DTSCH.MINER.GESELLSCH.REFERATE.DER.VORTRAEGE.; 1969(9), VOL. 47Miscellaneous

TEMPERATURABHAENGIGKEIT DER GITTERKONSTANTEN UND DER REFLEX-INTENSITAETEN VON ANORTHIT (INFLUENCE DE LA TEMPERATURE SUR LES CONSTANTES DU RESEAU ET L'INTENSITE DE LA REFLEXION DE L'ANORTHITE) (RESUME).CZANK M; LAVES F; SCHULZ H et al.1969; DTSCH.MINER.GESELLSCH.REFERATE.DER.VORTRAEGE.; 1969(9), VOL. 47Miscellaneous

INVESTIGATION OF DOMAINS IN ANORTHITE BY ELECTRON MICROSCOPY.CZANK M; SCHULZ H; LAVES F et al.1972; NATURWISSENSCHAFTEN; 1972, VOL. 59, NUM. 0002, P. 77Miscellaneous

TEMPERATURE DEPENDENCE OF DOMAINS IN ANORTHITECZANK M; VAN LANDUYT J; SCHULZ H et al.1972; NATURWISSENSCHAFTEN; DTSCH. ; 1972, VOL. 59, NUM. 0012, P. 646Serial Issue

TEMPERATURE DEPENDENCE OF DOMAINS IN ANORTHITECZANK M; VAN LANDUYT J; SCHULZ H et al.1972; NATURWISSENSCHAFTEN; DTSCH.; DA. 1972; VOL. 59; NO 12; PP. 646; BIBL. 5 REF.; 1 ILL.Serial Issue

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