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Bibliografia Baldelli C., Dal Piaz G.V., Polino R. (1983): Le quarziti a manganese e cromo di Varenche-St. Barthelemy, una sequenza di copertura oceanica della falda piemontese.

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Bibliografia

Baldelli C., Dal Piaz G.V., Polino R. (1983): Le quarziti a manganese e cromo di Varenche-St. Barthelemy, una sequenza di copertura oceanica della falda piemontese. Ofioliti, 8, 207-221.

Banno S., Higashino T., Otsuki M., Itaya T., Nakajima T. (1978): J. Phys. Earth, suppl., 26, 345-356.

Baretti M. (1893): Geologia della Provincia di Torino. Ed. F. Casanova, Torino.

Bearth P. (1967): Die Ophiolite der Zone von Zermatt-Saas Fee. Beitr. Geol. Karte Schweiz, Neue Folge 132, 1-130.

Bedognè F., Montrasio A., Sciesa E. (1993): I minerali della Provincia di Sondrio: Valmalenco. Bettini, Sondrio.

Bedognè F. & Sciesa E. (1995): I minerali di manganese della Val Malenco. Riv. Mineral. It., 19, 347-359.

Bedognè F., Maurizio R., Montrasio A., Sciesa E. (1995): I minerali della Provincia di Sondrio e della Bregaglia Grigionese: Val Bregaglia, Val Masino, Val Codera e Valle Spluga. Bettini, Sondrio.

Bermanec V., Armbruster T., Oberhaensli R., Zebec V. (1994): Crystal chemistry of Pb- and REE-rich piemontite from Nežilovo, Macedonia. Schweiz. Mineral. Petrogr. Mitt., 74, 321-328.

Bettendorff A. (1877): Über den Ardennit and über eine methode sur Scheidung der Vanadisaure von Thonerde und Eisenoxyd. Ann. Phys. Chem. Pogg., 160, 126-130.

Bogdański J. (1999): Historische Typ-Minerale in der Sammlung des Mineralogischen Museums der Universität von Wroclaw (Breslau). Aufschluss, 50, 305-320.

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Bonino A. (1948): Cenno preliminare sulle caratteristiche pegmatiti manganesifere delle Alpi Piemontesi. Atti del Congresso Minerario Italiano, Associazione Mineraria Sarda, Iglesias, 91-105.

Bonino A. (1965): Cenni petrografici su due giacimenti manganesiferi delle alpi piemontesi. Atti Rass. Tecn. Soc. Ing. Arch. Torino, 19, 613-616.

Brasseur H. (1930): Données nouvelles sur la structure de la dewalqnite et considérations sur sa composition chimique. C. R. Congrès Nat. Sci.Bruxelles, 1930, 144-146.

Brocker M. (1990): Die metamorphe vulkanosedimentare Abfolge der Insel Tinos (Kyklanden, Griechenland): Geologie, Petrographie und Mineralchemie einer grünschieferfaziell überprägten Hochdruck/Niedrigtemperatur-Abfolge. Geotekt. Forsch., 74, 107 p.

Brown I. D.& Shannon R.D. (1973): Empirical Bond-Strenght-Bond-Length curves of oxides. Acta Crystallogr., A29, 266-282.

Buttgenbach H. (1931-32): Sur un cristal de dewalquite. Ann. Soc. Géol. Belg., 55, B176.

Buttgenbach H. (1947): Les Minéraux de Belgique et du Congo Belge. Dunod Ed., Paris, H. Vaillant-Carmanne, S. A., Imp., Liège.

Castello P. (1981): Inventario delle mineralizzazioni a magnetite, ferro-rame e manganese del complesso piemontese dei calcescisti con pietre verdi in Valle d'Aosta. Ofioliti, 6, 5-46.

Cerri R. (1990): Quadro giacimentologico dell’alta Valsesia. In “Alagna e le sue miniere”, Pro Loco Alagna, CAI- Sez. Varallo Sesia, Sez. Archivio di Stato di Varallo Sesia, 79-99.

Cesàro G. (1909-10): Contribution à l'étude des minéraux. Ann. Soc. Géol. Belg., 37, 128-130.

Cesàro G. & Abraham A. (1908-09): La dewalquite. Ann. Soc. Géol. Belg., 36, 197-212.

Chopin C. (1978): Les paragènes réduites ou oxydées des concentrations manganésifères des "schistes lustrés" de Haute-Maurienne (Alpes françaises). Bull. Minéral., 101, 514-531.

(3)

Coombs D.S., Dowse M., Grapes R.H., Kawachi Y., Roser B.P. (1985): Geochemistry and origin of piemontite-bearing and associated manganiferous schists from Arrow Junction, Western Otago, New Zealand. Chem. Geol., 48, 57-78.

Coombs D.S., Kawachi Y., Reay A. (1993): An occurrence of ardennite in quartz veins in piemontite schist, Western Otago, New Zealand. Mineral. Petrol., 48, 295-308.

Corin F. (1927): Contribution à l'étude de la dewalquite. Ann. Soc. Géol. Belg., 51, B140.

Corin F. (1928): Un nouveau gite de dewalquite à Salmchâteau. Ann. Soc. Géol. Belg., 52, B27.

Dal Piaz G.V. (1969): Nuovo affioramento di quarziti e di scisti a piemontite in Valle d’Aosta. Boll. Soc. Geol. It., 88, 613-619.

Dal Piaz G.V., Di Battistini G., Kienast J.R., Venturelli G. (1979): Manganesiferous quarzitic schists of the Piemonte ophiolite nappe in the Valsesia-Valtournanche area (Italian Western Alps). Mem. Sci. Geol. Padova, 32, 24.

Deb M., Thorpe R.I., Cumming G.L., Wagner P.A. (1989): Age, source and stratigraphic implications of Pb isotope data for conformable, sediment-hosted, base metal deposits in the Proterozoic Aravalli-Dehli orogenetic belt, northwestern India. Precambrian Res., 43, 1-22.

De Koninck L.L. (1877): Petits cristaux accompagnant la dewalquite. Bull. Acc. Roy. Belg., 44, 740.

Donnay G. (1965): The structural relation of ardennite to epidote. Carnegie Inst. Washington Yb.,

1965, 209-210.

Donnay G. & Allmann R. (1968): Si3O10 groups in the crystal structure of ardennite. Acta

Crystallogr., B24, 845-855.

Donnay G. & Allmann R. (1971): Structural relation between pumpellyite and ardennite. Acta Crystallogr., B27, 1871-1875.

(4)

Dornberger-Schiff, K. (1966): Lehrgang über OD-Strukturen. Akademie-Verlag, Berlin, 135 p.

Embrey P.G. (1977): Fourth supplementary list of British minerals. Mineral. Mag., 42, 169-177.

Enami M. (1982): Oligoclase-biotite zone of the Sanbagawa metamorphic terrain in the Bessi district, central Shikoku, Japan. J. Geol. Soc. Japan, 88, 887-900.

Enami M. (1983): Petrology of the politic schists in the oligoclase-biotite zone of the Sanbagawa metamorphic terrain, Japan; phase equilibria in the highest zone of a high-pressure intermediate type of metamorphic belt. J. Metam. Geol., 1, 141-161.

Enami M. (1986): Ardennite in a quartz schist from the Asemi-gawa area in the Sambagawa metamorphic terrain, centrl Shikoku, Japan. Mineral J., 13, 151-160.

Fransolet A.M. (1982): Minéralogie de Belgique. Ardennite Mn2+(Mg,Al,Fe3+)

2Al4(As,V)O4(SiO4)2(Si3O10)(OH)6n. Bull. Soc. Belge Géol., 91, 50.

Galli E. & Alberti A. (1969): On the crystal structure of pumpellyite. Acta Crystallogr., B25, 2276-2281.

Geiger T. & Cabalzar W. (1989): Ardennit - ein Neufund von der Alp Parsettens. Schweizer Strahler, 8, 201-209.

Gennaro V. (1925): Micascisti a piemontite nelle Valli di Lanzo (Alpi Piemontesi). Rend. R. Acc. Naz. Lincei, Ser. 6, 2, 508-510.

Higashino T. (1975): Biotite zone of the Sanbagawa metamorphic terrain in the Shiragayama area, cental Shikoku, Japan. J. Geol. Soc. Japan, 81, 653-670.

Kawachi Y., Grapes R.H., Coombs D.S., Dowse M. (1983): Mineralogy and petrology of a piemontite-bearing schist, western Otago, New Zealand. J. Metam. Geol., 1, 353-372.

Lacroix A. (1893): Minéralogie de la France et des ses anciens territoires d'outre-mer. Vol. 1., Ristampa Librairie Rene Thomas, 1977, 124-127.

(5)

Lasaulx A. von (1872a): Vorläufige Mittheilung über ein neues Mineral (chemische Section. Sitzung vom 9 November). Ber. Niederrh. Gesell., 29, 174.

Lasaulx A. von (1872b): Über ein neues Mineral aus der Gegend von Ottrez (chemische Section. Sitzung vom 24 November). Ber. Niederrh. Gesell., 29, 189-192.

Lasaulx A. von (1872c): Ardennit, ein neues Mineral. N. Jb. Mineral., 1872, 930-934.

Lasaulx A. von (1873): Über den Ardennit. N. Jb. Mineral., 1873, 124-127.

Lasaulx A. von (1874): Über den Ardennit. N. Jb. Mineral., 1874, 276-278.

Lasaulx A. von (1876): XIII. Nachträge zur Kenntniss des Ardennites. N. Jb. Mineral., 1876, 363-368.

Lasaulx A. von & Bettendorf A. (1873) Ardennit, ein neues Mineral. Ann. Phys. Chem. Pogg., 149, 241-251.

Massonne H.J. & Chopin C. (1989): P-T history of the Gran Paradiso (Western Alps) metagranites based on phengite barometry. In “Evolution of metamorphic belts”, J.S. Daly, R.A. Cliff, B.W.D. Yardley, eds. Geol. Soc. London, Spec. Publ., 43, 545-549.

Matsubara S., Kato A. (1987): Ardennite from Sanbagawa in Sanbagawa metamorphic terrain, Kanto Mountains, Japan. Bull. Nat. Sci. Mus., Tokyo, ser. C, 13, 1-11.

Mellini M., Merlino S., Pasero, M. (1984): X-ray and HRTEM study of sursassite: crystal structure, stacking disorder, and sursassite-pumpellyite intergrowth. Phys. Chem. Minerals, 10, 99-105.

Mellini M., Merlino S., Pasero M. (1986): X-ray and HRTEM structure analysis of orientite. Am. Mineral., 71, 176-187.

Mélon J., Bourguignon P., Fransolet A.-M. (1976): Les minéraux de Belgique. Edition G. Lelotte, Belgium, 280 p.

(6)

Minakawa T. (1992): Study on characteristic mineral assemblages and formation process of metamorphosed manganese ore deposits in the Sanbagawa Belt. J. Fac. Sci. Ehime Univ., 1, 1-74.

Minakawa T. & Momoi H. (1987): Occurences of ardennite and sursassite from the metamorfic manganese deposit of the Sanbagawa Belt, Shikoku, Japan. J. Mineral. Soc. Japan, 18, 87-98.

Minakawa T., Momoi H., Noto S. (1986): Ardennite in a quartz vein in piemontite schist. Ann. Meet. Mineral. Soc. Japan, Nagoya, 50 (abstr) [in Japanese].

Momoi H. (1964):A new vanadium garnet, (Mn, Ca)3V2Si3O12, from the Yamato mine, Amami

Islands, Japan. Mem. Fac. Sci. Kyushu Univ., 15, 73-78.

Nayak V.K. (1963): Ardennite from India. Nature, 198, 778-779

Nayak V.K. (1966): Mineralogy and genesis of the manganese ores of Kajlidongri Mine, District Jhabua, Madhya Pradesh, India. Econ. Geol., 61, 1280-1282

Nayak V.K. (1967): Ardennite from Kajlidongri, India: a new locality. N. Jb. Mineral. Mh., 1967, 295-304.

Nayak V.K. (1973): Relations of quartz veins to epithermal minerals of Kajilidongri Mine, District Jhabua, M.P. In “Orogenesis and Metallogenesis in the Precambrian of India”, Indian School of Mine, Dhanbad, 14 (abstr.).

Nayak V.K. (1980): The manganese ore of Kajlidongri, District Jhuabua, Madhya Pradesh, India. In “Geology and Geochemistry of Manganese, Vol. II“, I.M. Varentsov & G.Y. Grasselly, eds. E. Schweizerbart'sche Verlagsbuchhandlung, Stuttgart, 265-277.

Nevenka A. (1992): Crystallochemical characteristic of minerals from barium silicate-cintaining parageneses. Prirodoslovno-matematièki fakultet, Mineraloško-petrografski zavod Zagreb, 163 p.

(7)

Pasero M., Reinecke T., Fransolet A.-M. (1994): Crystal structure refinements and compositional control of Mn-Mg-Ca ardennites from the Belgian Ardennes, Greece, and the Western Alps. N. Jb. Mineral. Abh., 166, 137-167.

Pelloux A. (1922): Miniere e minerali manganesiferi della Val d’Aosta. Rend. Lavori Uff. Invenzioni Ricerche Roma, 1, 22-38.

Pelloux A. (1946): Contributo alla mineralogia della Valle d’Aosta (Ardennite della miniera di Varenche presso S. Barthelemy). Rend. Soc .Mineral. It., 3, 188-206.

Peters T., Trommsdorff V., Sommerauer J. (1978): Manganese pyroxenoids and carbonates: critical phase relations in metamorphic assemblages from the Alps. Contrib. Mineral. Petrol., 66, 383-388.

Pisani F. (1872): Sur un nouveau silico-aluminate de manganèse vanadinifère, trouvé à Salm Château, en Belgique. C. R. Acad. Sci. Paris, 75, 1542-1544.

Pisani F. (1873): Analyse de la dewalquite de Salm-Château en Belgique. C. R. Acad. Sci. Paris,

77, 329-333.

Prantl W. (1905): Über den Ardennit. Z. Kristallogr., 40, 392-395.

Reinecke T. (1986): Phase relationships of sursassite and other Mn-silicates in highly oxodized low-grade, high pressure metamorphic rocks from Evvia and Andros islands, Greece. Contrib. Mineral. Petrol., 94, 110-126.

Reinecke T. (1989): Mg-P-Si rich ardennite: a high pressure phase in eclogite-facies piemontite quarzites from Cignana, Valtournanche, western Alps. Terra Abstr., 1, 20-21.

Reinecke T. (1991): Very high pressure metamorphism and uplift of coesite-bearing metasediments from the Zermatt-Saas zone, western Alps. Eur. J. Mineral., 3, 7-17.

(8)

Reinecke T. & Hatzipanagiotou K. (1987): Crystal chemistry and lattice parameters of ardennites from Andros island, Greece, and Haute-Maurienne, Western Alps. N. Jb Miner. Abh., 158, 89-104.

Reinecke T., Okrusch M., Richter P. (1985): Geochemistry of ferromanganoan metasediments from Andros island, Cycladic blueschist belt, Greece. Chem. Geol., 53, 249-278.

Sciesa E. (1987): Studio geologico- petrografico e mineralogico della Zona Lanzada-Scermendone (Val Masino-Val Malenco). Tesi di Laurea, Univ. Milano, 330 p.

Semet M. & Moreau J. (1965): L'ardennite: révision et données nouvelles. Ann. Soc. Géol. Belg.,

88, 545-577.

Shannon R.D. (1976): Revised effective ionic radii and systematic studies on interatomic distances in halides and chalcogenides. Acta Crystallogr., A32, 751-767.

Shannon R.D. & Prewitt C.T. (1969): Effective ionic radii in oxides and fluorides. Acta Crystallogr., B25, 925-945.

Stelzner A.W. & Bergeat A. (1904): Die Erzlagerstätten. Leipzig

Strunz H. (1935): Strukturelle und morphologische Beziehungen zwischen Epidot und Zoisit und zwischen Epidot und Ardennit. Z. Kristallogr., 92, 402-407.

Wenk H.RT. & Maurizio R. (1978): Kutnahorite, a rare Mn mineral from Piz Cam (Bergell Alps). Schweiz. Mineral. Petrogr. Mitt., 58, 97-100.

Yoshimura T. and Momoi H. (1964): Vanadium silicate minerals from the Yamato mine, Kagoshima Prefecture, Japan. Sci. Rep. Imp. Kyushu Univ., Geol. Ser., 7, 85-90 [in giapponese; riassunto in Mineral. Abstr., 17, 183 (1965)].

Zambonini F. (1922): Ardennite di Ceres in Val d’Ala (Piemonte). Rend. R. Acc. Naz. Lincei, ser. 5,

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