TWO EPISODES OF HIGHGRADE METAMORPHISM IN THE NORTHERN BERGELL ALPS.WENK HR.1974; SCHWEIZ. MINERAL. PETROGR. MITT.; SCHWEIZ; 1974, VOL. 54, NUM. 0002-0003, P. 555 A 565Serial Issue

GEOLOGISCHE BEOBACHTUNGEN IM BERGELL. I. GEDANKEN ZUR GENESE DES BERGELLER GRANITS. RUECKBLICK UND AUSBLICK (REMARQUES GEOLOGIQUES DANS LE MASSIF DE BERGELL. IDEES CONCERNANT LA GENESE DU GRANITE DE BERGELL. COUP D'OEIL RETRASPECTIF ET PERSPECTIVE).WENK HR.1970; SCHWEIZ. MINER. PETROGR. MITT.; 1970, VOL. 50, NUM. 0002, P. 321 A 348Miscellaneous

SUBMICROSCOPICAL TWINNING IN LUNAR AND EXPERIMENTALLY DEFORMED PYROXENES.WENK HR.1970; BEITR. MINERAL PETROL; DEU; 1970, VOL. 26, NUM. 0004, P. 315 A 323Miscellaneous

THE GEOLOGY OF THE BERGELL MASSIV. REVIEW AND PREVIEW (ABSTRACT).WENK HR.1969; DTSCH.MINER.GESELLSCH.REFERATE.DER.VORTRAEGE.; 1969(9), VOL. 47, P. 60 A 61Miscellaneous

MULLITE-SILLIMANITE INTERGROWTH FROM PELITIC INCLUSIONS IN BERGELL TONALITE = TEXTURE SYMPLECTIQUE MULLITE-SILLIMANITE DES INCLUSIONS PELITIQUES DANS LA TONALITE DE BERGELLWENK HR.1983; NEUES JAHRB. MINERAL., ABH.; ISSN 0077-7757; DEU; DA. 1983; VOL. 146; NO 1; PP. 1-14; BIBL. 19 REF.; ILL./ESQUISSE GEOL.Article

SOME ROOTS OF EXPERIMENTAL ROCK DEFORMATIONWENK HR.1979; MECANISMES DE DEFORMATION DES MINERAUX ET DES ROCHES. CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE. COLLOQUE INTERNATIONAL. 290/1978-10-01/PERROS-GUIREC; FRA; PARIS: CNRS; DA. 1979; PP. 195-202; ABS. FRE; BIBL. 49 REF.Conference Paper

SUPERSTRUCTURE VARIATION IN METAMORPHIC INTERMEDIATE PLAGIOCLASEWENK HR.1979; AMER. MINERALOGIST; USA; DA. 1979; VOL. 64; NO 1-2; PP. 71-76; BIBL. 18 REF.; 4 ILL.Article

AN ALBITE-ANORTHITE ASSEMBLAGE IN LOW-GRADE AMPHIBOLITE FACIES ROCKSWENK HR.1979; AMER. MINERALOGIST; USA; DA. 1979; VOL. 64; NO 11-12; PP. 1294-1299; BIBL. 19 REF.Article

HOWIEITE, A NEW TYPE OF CHAIN SILICATE.WENK HR.1974; AMER. MINERALOGIST; U.S.A.; DA. 1974; VOL. 59; NO 1-2; PP. 86-97; BIBL. 10 REF.; 8 ILL.Article

VARIATIONS OF LATTICE CONSTANTS IN CLINOAMPHIBOLES.WENK HR.1971; Z. KRISTALLOGR.; DEU; 1971, VOL. 133, P. 341 A 363Miscellaneous

SUBMICROSCOPICAL TWINNING IN LUNAR AND EXPERIMENTALLY DEFORMED PYROXENES.WENK HR.1970; BEITR. MINERAL PETROL; DEU; 1970, VOL. 26, NUM. 0004, P. 315 A 323Miscellaneous

THE GEOLOGY OF THE BERGELL MASSIV. REVIEW AND PREVIEW.WENK HR.1970; FORTSCHR. D. MINERAL.; DEU; 1970(5), VOL. 47, NUM. 0001, P. 76 A 78Miscellaneous

ANNEALING OF OLIGOCLASE AT HIGH PRESSURE.WENK HR.1969; AMER.MINERALOGIST.; 1969(2), VOL. 54, P. 95 A 100Miscellaneous

THE CRYSTAL STRUCTURES OF YTTRIUM, HOLMIUM AND ERBIUM FORMATE DIHYDRATESWENK HR.1981; Z. KRISTALLOGR.; ISSN 0044-2968; DEU; DA. 1981; VOL. 154; NO 1-2; PP. 137-145; BIBL. 13 REF.Article

DEFECTS ALONG KYANITE-STAUROLITE INTERFACES = DEFAUTS AUX INTERFACES KYANITE-STAUROLITEWENK HR.1980; AM. MINERAL.; ISSN 0003-004X; USA; DA. 1980; VOL. 65; NO 7-8; PP. 766-769; BIBL. 6 REF.; ILL.Article

ORDERING OF THE INTERMEDIATE PLAGIOCLASE STRUCTURE DURING HEATING.WENK HR.1978; AMER. MINERALOGIST; U.S.A.; DA. 1978; VOL. 63; NO 1-2; PP. 132-135; BIBL. 1 P.; 2 ILL.Article

POLYMORPHISM OF WOLLASTONITE.WENK HR.1969; BEITR. MINERAL PETROL; DEU; 1969, VOL. 22, NUM. 0003, P. 238 A 247Miscellaneous

ANNEALING EXPERIMENTS OF OLIGOCLASE.(ABSTRACT).WENK HR.1968; GEOL. SOC. AMER., ABSTR. PROGRAMS; USA; 1968Miscellaneous

MULLITE-SILLIMANITE INTERGROWTH FROM PELITIC INCLUSIONS IN BERGELL TONALITEWENK HR.1983; NEUES JAHRBUCH FUER MINERALOGIE. ABHANDLUNGEN; ISSN 0077-7757; DEU; DA. 1983; VOL. 146; NO 1; PP. 1-14; BIBL. 18 REF.Article

MORE PORPHYRITIC DIKES IN THE BERGELL ALPS = DYKES PORPHYRIQUES DANS LES ALPES BERGELLWENK HR.1980; SCHWEIZ. MINERAL. PETROGR. MITT.; ISSN 0036-7699; CHE; DA. 1980; VOL. 60; NO 2-3; PP. 145-152; BIBL. 21 REF.Article

A GEOLOGICAL HISTORY OF BERGELL GRANITE AND RELATED ROCKS = HISTOIRE GEOLOGIQUE DU GRANITE DE BERGELL ET DES ROCHES QUI LUI SONT LIEESWENK HR.1982; TRANSFORMISTS' PETROLOGY; GRC; ATHENS: THEOPHRASTUS; DA. 1982; PP. 113-148; BIBL. 5 P.; ESQUISSE GEOL./COUPE GEOL./ILL.Book Chapter

SOME ROOTS OF EXPERIMENTAL ROCK DEFORMATION = SUR LES ORIGINES DE LA DEFORMATION EXPERIMENTALE DES ROCHESWENK HR.1979; BULL. MINERAL.; FRA; DA. 1979; VOL. 102; NO 2-3; PP. 195-202; ABS. FRE; BIBL. 49 REF.; 7 ILL.Article

ARE PSEUDOTACHYLITES PRODUCTS OF FRACTURE OR FUSION.WENK HR.1978; GEOLOGY; U.S.A.; DA. 1978; VOL. 6; NO 8; PP. 507-511; BIBL. 25 REF.; 7 ILL.Article

STRUCTURE, FORMATION, AND DECOMPOSITION OF APB'S IN CALCIC PLAGIOCLASEWENK HR; NAKAJIMA Y.1980; PHYS. CHEM. MINER.; DEU; DA. 1980; VOL. 6; NO 3; PP. 169-186; BIBL. 2 P.; 8 ILL.Article

CHANGES IN THE DOMAIN STRUCTURE OF ANORTHITES INDUCED BY HEATINGMULLER WF; WENK HR.1973; NEU. JB. MINERAL., MONATSH.; DTSCH.; DA. 1973; NO 1; PP. 17-26; BIBL. 1 P.Serial Issue