Postl, W. & Moser, B. c, d Eclogite. Geological Survey of Western Australia, Mineral Resources Bulletin 15. The field of view is about 2.5 mm. (1991): Pegmatittmineraler fra Larvik ringkompleks. Rocks & Min 70:5 pp 320-333; Am. Plotinskaya, O. Y., Abramova, V. D., Groznova, E. O., Tessalina, S. G., Seltmann, R., & Spratt, J. Theye, T., Fransolet, A.-M. (1994) Virtually Pure Ottrelite from the Region of Ottré, Belgium. Northrop, Minerals of New Mexico, 3rd Rev. Each thin section was first scanned in unpolarized light and then again between two sheets of crossed polaroid film aligned parallel to the thin section edges. Thin section of massive fine-grained talc replacing coarse dolomite in crossed polarized light. (1988): Mineralogische Notizen aus der Steiermark. Ofioliti, 14, 135-156. Stöckhert, Bernard, Johannes Duyster, Claudia Trepmann, Hans-Joachim Massonne (2001), Microdiamond daughter crystals precipitated from supercritical COH & plus; silicate fluids included in garnet, Erzgebirge, Germany: Geology: 29(5): 391-394. Economic Geology 111, 619-639. Philippe Roth, Ed., Zurich, 239 pp. Quinn, A. W. and H. D. Glass (1958): Rank of coal and metamorphic grade of rocks of the Narragansett Basin of Rhode Island (Economic Geology 53(5): 563-576). Max, M.D., Treloar, P.J., Winchester, J.A. 5(1):31. Min. Type I and II garnet grains coexist in thin sections of samples QE9601 and QE9602. Contributions to Mineralogy and Petrology, 158, #1, 1-16.; Cárdenas-Párraga, J., García-Casco, A., Núñez-Cambra, K., Rodríguez-Vega, A., Blanco-Quintero, I. F., Harlow, G. E., & Lázaro, C. (2010). Deer, FRS, R. A. Howie, J. Zussman. Kramm, U. Raymond M. Coveney Gold quartz veins and auriferous granite at the Oriental Mine, Alleghany District, California Economic Geology and the Bulletin of the Society of Economic Geologists (December 1981), 76(8):2176-2199. American Mineralogist 49, 183-190. (2000): Mineralium Deposita 35, 233-259. Field of view is 1.5 cm. , 1985, 108, pp. Paragonite NaAl2(Si3Al)O10(OH)2 °c 20 1M i nera lD t Pub sh g, v o . p 96. 63, 1 map, British Geological Survey publ., Nottingham. Possibly some andalusite is still present in a few of the pseudomorphs, but this could not be confirmed in thin section due to the ubiquitous presence of fine-grained margarite. Sample QE9601 is a typical kyanite‐bearing quartz eclogite. Dal Piaz, G.V., Gianotti, F., Monopoli, B., Pennacchioni, G., Tartarotti, P., Schiavo, A., with contributions of Carraro, F., Bistacchi, A., Massironi, M., Martin, S., Ratto, S., (2008) Note illustrative della Carta geologica d’Italia alla scala 1:50.000, foglio 091, Châtillon. 24 pp. Important correlations between these aspects of mineralogy are emphasized wherever possible. Schweizerische Mineralogische und Petrographische Mitteilungen, 81(3), 369-378. Paragonite in the Schist of Glebe Mountain, Southern Vermont (Am Min 41:144-147). Grabezhev, A. I., Pertsev, N. N., Zadov, A. E., Pribavkin, S. V., & Murzin, V. V. (2007). The content of each section has been updated where needed in the light of published research over the 21 years between editions. Guo, W., Li, J., Wang, Z., Zhang, K., Gao, Z., Ma, J., Zhao, C. (2020): Mineralogical Characteristics of Early Permian Paragonite-Bearing Coal (No. No information on health risks for this material has been entered into the database. Cheney and Guidotti, Am Min 58: 1076-1079. Mines & Minerals 13:16-55. Sabina, Ann P. (2003) Rocks and minerals for the collector: Kirkland Lake - Rouyn-Noranda - Val-d'Or, Ontario and Quebec. (2011) Prograde lawsonite during the flow of continental crust in the Alpine subduction: Strain vs. metamorphism partitioning, a field-analysis approach to infer tectonometamorphic evolutions (Sesia-Lanzo Zone, Western Italian Alps). ‎Biaxial Minerals in Thin Section volume 3a is an atlas of the optical and ancillary physical properties of biaxial minerals observable by transmitted light microscopy. Geology, 33(10), 761-764. Ford, T., A. Sarjeant & M. Smith (1993) The minerals of the Peak district of Derbyshire UK Jour. Bearth, P. (1963): Chloritoid und Paragonit aus der Ophiolit-Zone von Zermatt-Saas Fee. 2ème édition, Muséum des Sciences Naturelles, Bruxelles, Belgium, 304 pages (in French). & Berger, A. Paragonite and margarite often cannot be distinguished from muscovite in thin section. Lishmund, S.R. Lithos, 103(1-2), 106-137. Journal of Petrology, 8, 349-371. (2002). Ryback, G., Nawaz, R. and Farley, E. (1988) Seventh Supplementary List of British Isles Minerals (Irish). Wepf Verlag, Basel, pages 261-262; Roth, Ph. Reed, Juliet C. (1976), Annotated Biblio. Novák, M. & Škoda, R. (2007): Mn3+-rich andalusite to kanonaite and their breakdown products from metamanganolite at Kojetice near Třebíč, the Moldanubian Zone, Czech Republic. Corundum, Cr-muscovite rocks at O'Briens, Zimbabwe: the conjunction of hydrothermal desilicification and LIL-element enrichment—geochemical and isotopic evidence. The chemical composition of paragonite differs from that of muscovite in that sodium replaces potassium. California Division of Mines and Geology, County Report 3: p 89., illus., maps. Pp. 47, n° 344, pp. Alteration of calcium-and aluminium-rich inclusions in the Murray (CM2) carbonaceous chondrite. 178-181 in Walter, F. et al. Muscovitic mica and chlorite are common alteration components in porphyry Cu-Mo deposits. Preiswerkite, Ca-(Mg, Fe)-paragonite and Ca-“ephesite” in metadiorite from the HP Kechros Metamorphic Complex in Eastern Rhodope, NE Greece. G. Niedermayr, I. Praetzel: Mineralien Kärntens, 1995, Bottrill, R.S., Baker, W.E. Published by M. Blondieau, Tellin, Belgium, 90 pp. Mitt., 81, 379-393. Canadian Mineralogist 38, 707-712. Goffé, B. (2014). ... member, and Paragonite showing compositions between about 80% and 100% of the Na-rich Guidotti, C.V., Sassi, F.P., Comodi, P., Zanazzi, P.F., Blencoe, J.G. Kullerud, K., Nasipuri, P., Ravna, E. J. K., & Selbekk, R. S. (2012) Formation of corundum megacrysts during H2O-saturated incongruent melting of feldspar: P–T pseudosection-based modelling from the Skattøra migmatite complex, North Norwegian Caledonides. Associazione Amici del Museo "F. Eusebio" di Alba, Ed., Alba, 137-139. Jambor, J.L., Pertsev, N.N., and Roberts, A.C. (1999) New mineral names. Plotinskaya, O. Y., Grabezhev, A. I., Groznova, E. O., Seltmann, R., & Lehmann, B. New to the PA List 1965-1974, The Mineralogical Soc. Sci., Vol. Crystal Data: Monoclinic; hexagonal in part. and Oppenheim, M.J. (1983) Cr Mica from the Precambrian Erris Complex, NW Mayo, Ireland. Textural and spatial relationship between platinum-group elements and alteration assemblages in the Afton porphyry system, Kamloops, British Columbia.