General Index Rut – Sch

Total Page:16

File Type:pdf, Size:1020Kb

General Index Rut – Sch GENERAL INDEX RUT – SCH QUADRIDAVYNE Bahia Inca de Oro: drusy quartz on chrysocolla Relations to other cancrinite-group minerals Brumado mine: 12-cm prisms including he- 26:492n 27:110q matite and goethite 28:137n; 5.6-cm speci- China Italy men with Japan-law twin 31:44p Feng Jiashan mine, Daye: Japan-law twins to Campania Fazenda Recruta, Vitoria de Conquista: very 4 x 5 cm 35:156n Mte. Somma/Vesuvius 27:(110), 27:460 dark smoky crystals to 15 cm 28:60n Gimkohe: doubly terminated crystals to 25 cm 34: QUARTZ Espirito Santo with acicular inclusions 186n Mimoso do Sul mine, Santa Teresa: huge Hichang quarry, Sichuan: pale red, hematite- Amethyst. Werner Lieber. 26:232–233b smoky quartz crystals with topaz 26:TZ23 stained transparent crystals 34:283n “Quartz case” at 1996 Tucson Show 27:222 Minas Gerais Jiangxi: transparent hematite-dusted red crys- Quartz chromophors, “pink” vs. “rose” quartz Aricanga pegmatite, Cruzeiro area: large crys- tals with hematite rosettes 31:283n (abstract) 32:42 tals with green elbaite 35:253n Jinkouhe, Sichuan: doubly terminated transpar- Quarz-Monographie. Die Eigenheiten von Berg- Corinto: crystals with rutile and brookite ent crystals to 5 cm 33:99n kristall, Rauchquarz, Amethyst, Chalcedon, inclusions 35:156n Nanchan, Jansee: crystals with hematite phan- Achat, Opal und anderen Varietäten. R. Rykart. Diamantina: tabular crystals with fadens toms and coatings 28:137n 29:507–508b 26:490n; crystals with pyrite inclusions Shang Bao mine, Leiyang, Hunan: sceptered Rykart’s descriptions of “Bambauer” and “Fried- 28:413n milky crystals in large groups 32:256n; scep- lander” crystals 35:403–404 Jaboti mine, São Geraldo do Baixio: com- ters with pyrite 32:497n Afghanistan plex “cathedral” crystals 26:490n,c Shangping Zhen, Longchuan County, Guang- Bamiyan Province: translucent amethyst crys- Lavra Berilo Branco: spectacular rose quartz dong: transparent prismatic hematite-stained tals to 8 cm 32:497n crystal specimens 30:No. 5 (cover), crystals, deep red, to large sizes 34:283n Paroon: dark pink rose quartz crystals on color- 30:361–365h,p Sichuan province: scepter specimens with 2.5- less quartz prisms 33:264p, 274n Lavro do Sapo: fine crystal groups 31:104n cm heads 31:509n Argentina Locality not specified: 60-cm scepter crystal Czech Republic Clavero mine, Corboda: 6.1-cm amethyst crys- 35:150n Cicov Hill, Horonec, near Bilina, Bohemia: tal 34:85p; amethyst scepter crystals 34:188n Macaco mine: multi-hued parallel growth gray chalcedony veins 35:142 Papachacra, Catamarca: smoky quartz in peg- crystals to 15 cm 26:490n,c England matite 31:99 São Geraldo do Baixio: small milky crystals Cumbria Australia with brazilianite 28:417n Brownley Hill mine, Alston Moor: milky Northern Territory Sapucaia pegmatite, Galiléia: colorless to white pyramidal crystals to 5 cm 31:247 Entia Valley, Harts Range: scepter amethyst pale smoky crystals to 10 cm 30:359 Yorkshire crystals 33:515–521c,d,p Paraíba Boulby mine, Loftus, Cleveland: drusy crys- Victoria Santana de Mangeiras: amethyst scepters with tal crusts in boracite nodules 27:169 Morella: sharp, bright, zoned smoky crystals milky bases to 5 cm 31:180 Ethiopia 27:139p, 144n Rio Grande do Sul Konzo, Sidamo: pale smoky crystals with mi- Austria Irai region: huge amethyst geodes with cal- crocline 35:156n Salzburg cite, gypsum 31:182q France Habachtal: transparent colorless skeletal crys- Bulgaria Chamonix: smoky crystals, gwindels 34:87n tal 1.3 meters long 34:188n 17th of September mine, Madan: large plate of Isère: miniature gwindel specimens 35:156n Rauris, Hohe Tauern: huge scepter specimen needle quartz 34:87n La Combe de la Selle, Isère: transparent prisms 34:186p Droukouvo mine, Laki, Rhodope Mts.: casts to 5 cm 32:228 Azerbaijan after calcite crystals to 5 cm 32:497n La Gardette mine, Isére: groups of very thin Dashkesan: amethystine, in bowtie-shaped clus- Kruchov Dol mine, Madan district: flattened colorless prisms 31:277n ters 27:452n; prisms to 12 cm 28:508n; small Japan-law twins 34:275n Mont Blanc area: smoky quartz, gwindels, crystals with apatite and galena 34:186n Madan district: cluster with Japan-law twin fadens, all sizes 31:277n Bolivia 32:58n Oisans: 10 x 10-cm crystal with chlorite phan- Ani mine, Santa Cruz Department: 10-cm Canada toms 35:148n “ametrine” crystals 26:489n British Columbia Pierre Joseph Peak near Mer de Glace, Arrahi, near Puerto Suarez: amethyst crystal Dunn Peak, south of Clearwater: smoky Chamonix: lustrous faden smoky crystals in clusters to 45 cm 30:218n quartz, amethyst 26:491 plates to 15 cm 34:281n Ayoreita mine, Rincón del Tigre, Santa Cruz: Engineer mine, Tagish Lake: pseudomorphs Ribiero & Orpierre, Hautes Alpes: Herkimer- amethyst druses to 50 cm 30:153n after calcite 27:269n,p like crystals 26:221p, 223n Cerro Rico de Potosí, Potosí: massive, small Passmore area: smoky quartz with spessartine, Sigoyer, Haute Provence: flawless colorless crystals, chalcedony 30:31 beryl 26:491; Japan-law twins to 5 cm crystals to 6 cm 28:135p, 137n Chambillaya mine: Japan-law twins 34:116 26:578n Tour Noir, Argentiere, Chamonix, Haute-Savoie: Chicote Grande mine: Japan-law twins to 10 Silvana mine, Sandon: colorless crystals to gemmy smoky prisms to 6 cm with octahe- cm with ferberite 34:116 1.5 cm, unusual habits 27:437 dral pink fluorite 29:129n, 131p Kami mine, Cochabamba: Japan-law twins to Slocan area: Japan-law twins to 5 cm 26:491 Trimouns quarry, Luzenac, Ariège: fine trans- 1.5 cm coating matrix 29:213n; Japan-law Ontario parent crystals to 35 cm 35:241p twins to 8 cm with sulfides 34:116 Diamond Willow mine, Thunder Bay: large Greece Locality not specified: phantom amethyst in plates of hematoid amethyst 29:128n Avessalos, Seriphos: aesthetic specimens of very large crystal groups 35:160n Quebec green quartz 31:99n Pacajake mine, Potosí: veinlets near mine 34:354 Lac Nicolet mine, South Ham: Herkimer-like Locality not specified: crystals to 7.5 cm in Rincon de Tigre, north of Ani mine, Santa Cruz microcrystals, some larger 27:128 clusters to 15 x 50 cm 34:85n Department: Herkimer-like crystals with 3- Mines Cristal Kebec (formerly Adams farm Seriphos Island (green) 26:(99) phase fluid inclusions, hydrocarbons 26:489n prospect): transparent crystals 26:491 Hungary Siglo XX mine, Llallagua: Japan-law twins to 5 Mont St.-Hilaire: Japan-law, Dauphiné twins Chemnitz: crystals on matrix, Ferguson collec- cm 34:116 in micromounts 34:180–181p tion 31:432p Tasna mine: Japan-law twins 34:116 Saint-Amable sill: microcrystals, chalcedony Rudabánya: drusy cavity linings, crystals to 1 Bosnia/Hercegovina 29:106 cm 32:126 Zagradski Potok near Busovac=a: crystals to 12 Yukon Territory India cm including twins, fadens, etc. 27:342– Scepter claim near Emerald Lake, Hess Moun- Bombay area, Maharashtra: cavity-lining druses, 343p, 344–346c tains: sceptered smoky 26:491n rare crystals to 5 cm 34:58, 70 Brazil Chile Deccan Plateau: general locality survey 34:58 Serro do Cabral: Japan-law twins to 10 x 10 cm El Indio, Coquimbo: encrustation pseudomor- Jalgaon, Maharashtra: chalcedony and drusy 34:188n phs after enargite 26:492n quartz with zeolites 34:73 The Mineralogical Record Index—Volumes 26–35 107 SCH – SCO GENERAL INDEX Karur, Tamil Nadu: sceptered amethyst crystals Durango Shigar region: small, highly lustrous crystals 28:212n; large plates of deep purple am- Mapimí district: slightly corroded crystals, 28:137n ethyst crystals 31:282n, 284p amethystine crystals to 1 cm 34:OJ81 Shigar Valley: rose quartz crystals in flower- Kurar quarry, Bombay-Malad, Maharashtra: Guanajuato like 3.5-cm cluster 27:222n prismatic crystals to 10 cm, tabular crystals Valenciana mine, Veta Madre: colorless, Toyee, South Waziristan: “faden” floaters in with zeolites 34:58, 70 amethystine with calcite 26:496n miniature, small-cabinet sizes 30:53n Shirdi, Maharashtra: cavity-lining amethyst crys- Guerrero Wama, Dara Ismael, Khan district, NWFP: tals with okenite 34:57p, 77 Amatitlan: spindle-shaped amethyst crystals loose, colorless, transparent crystals to 5 cm Ireland to 10 cm 28:137n; fine 12.2-cm group with organic inclusions 34:282n Silvermines district, County Tipperary: slender 35:No. 6 (cover); complete description of Wanna, Waziristan, Northwest Frontier Prov- colorless prisms to 3 cm 30:103 locality 35:GU29–37h,p ince: skeletal, clay-included crystals to 12 Italy Chilpancingo: smoky crystals to 4 cm 26:222n cm 32:55n Liguria La Valenciana mine, Amatitlan: deep purple Waziristan: “faden” crystals 30:150n Val Graveglia: crystals to 8 cm 32:370p, 372 amethyst crystals to 12 cm 27:456n Zagi Mountain, Northwest Frontier Province: Piemonte Locality not specified: 12-cm crystals with transparent crystals to 15 cm, some with Vinadio: transparent crystals, some fadens orange-brown calcite crystals 28:505n; dark astrophyllite/riebeckite inclusions 35:218– 34:201 purple crystals to 12 cm 34:186n; crystals 219p Tuscany to 15 cm 35:156n Peru Carrara quarries: Herkimer-like crystals San Luis Potosi Alimon mine, Huaron: Japan-law twins with 31:510n Charcas: pale amethyst, Japan-law twinned sphalerite, chalcopyrite 34:116; 34:(248) Rio Marina, Elba: green quartz 27:451p 27:452n Cantera Raurita mine, Ancash Dept.: smoky Japan La Aurora mine, Charcas: citrine crystals on crystals to 12 cm 29:213n Narushima, Nagasaki Prefecture, Kyushu: Japan- danburite 28:205n Casapalca district, Lima Dept.: druses, milky to twin locality closed 26:495n; fine thumbnail Taman: doubly terminated crystals to 2.5 cm colorless crystals 28:P82 Japan-law twins recently collected 31:283n
Recommended publications
  • An Application of Near-Infrared and Mid-Infrared Spectroscopy to the Study of 3 Selected Tellurite Minerals: Xocomecatlite, Tlapallite and Rodalquilarite 4 5 Ray L
    QUT Digital Repository: http://eprints.qut.edu.au/ Frost, Ray L. and Keeffe, Eloise C. and Reddy, B. Jagannadha (2009) An application of near-infrared and mid- infrared spectroscopy to the study of selected tellurite minerals: xocomecatlite, tlapallite and rodalquilarite. Transition Metal Chemistry, 34(1). pp. 23-32. © Copyright 2009 Springer 1 2 An application of near-infrared and mid-infrared spectroscopy to the study of 3 selected tellurite minerals: xocomecatlite, tlapallite and rodalquilarite 4 5 Ray L. Frost, • B. Jagannadha Reddy, Eloise C. Keeffe 6 7 Inorganic Materials Research Program, School of Physical and Chemical Sciences, 8 Queensland University of Technology, GPO Box 2434, Brisbane Queensland 4001, 9 Australia. 10 11 Abstract 12 Near-infrared and mid-infrared spectra of three tellurite minerals have been 13 investigated. The structure and spectral properties of two copper bearing 14 xocomecatlite and tlapallite are compared with an iron bearing rodalquilarite mineral. 15 Two prominent bands observed at 9855 and 9015 cm-1 are 16 2 2 2 2 2+ 17 assigned to B1g → B2g and B1g → A1g transitions of Cu ion in xocomecatlite. 18 19 The cause of spectral distortion is the result of many cations of Ca, Pb, Cu and Zn the 20 in tlapallite mineral structure. Rodalquilarite is characterised by ferric ion absorption 21 in the range 12300-8800 cm-1. 22 Three water vibrational overtones are observed in xocomecatlite at 7140, 7075 23 and 6935 cm-1 where as in tlapallite bands are shifted to low wavenumbers at 7135, 24 7080 and 6830 cm-1. The complexity of rodalquilarite spectrum increases with more 25 number of overlapping bands in the near-infrared.
    [Show full text]
  • Metamorphism of Sedimentary Manganese Deposits
    Acta Mineralogica-Petrographica, Szeged, XX/2, 325—336, 1972. METAMORPHISM OF SEDIMENTARY MANGANESE DEPOSITS SUPRIYA ROY ABSTRACT: Metamorphosed sedimentary deposits of manganese occur extensively in India, Brazil, U. S. A., Australia, New Zealand, U. S. S. R., West and South West Africa, Madagascar and Japan. Different mineral-assemblages have been recorded from these deposits which may be classi- fied into oxide, carbonate, silicate and silicate-carbonate formations. The oxide formations are represented by lower oxides (braunite, bixbyite, hollandite, hausmannite, jacobsite, vredenburgite •etc.), the carbonate formations by rhodochrosite, kutnahorite, manganoan calcite etc., the silicate formations by spessartite, rhodonite, manganiferous amphiboles and pyroxenes, manganophyllite, piedmontite etc. and the silicate-carbonate formations by rhodochrosite, rhodonite, tephroite, spessartite etc. Pétrographie and phase-equilibia data indicate that the original bulk composition in the sediments, the reactions during metamorphism (contact and regional and the variations and effect of 02, C02, etc. with rise of temperature, control the mineralogy of the metamorphosed manga- nese formations. The general trend of formation and transformation of mineral phases in oxide, carbonate, silicate and silicate-carbonate formations during regional and contact metamorphism has, thus, been established. Sedimentary manganese formations, later modified by regional or contact metamorphism, have been reported from different parts of the world. The most important among such deposits occur in India, Brazil, U.S.A., U.S.S.R., Ghana, South and South West Africa, Madagascar, Australia, New Zealand, Great Britain, Japan etc. An attempt will be made to summarize the pertinent data on these metamorphosed sedimentary formations so as to establish the role of original bulk composition of the sediments, transformation and reaction of phases at ele- vated temperature and varying oxygen and carbon dioxide fugacities in determin- ing the mineral assemblages in these deposits.
    [Show full text]
  • 1 CRYSTAL CHEMISTRY of SELECTED Sb, As and P MINERALS
    Crystal Chemistry of Selected Sb, As, and P Minerals Item Type text; Electronic Dissertation Authors Origlieri, Marcus Jason Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 07/10/2021 10:49:41 Link to Item http://hdl.handle.net/10150/194240 1 CRYSTAL CHEMISTRY OF SELECTED Sb, As AND P MINERALS by Marcus Jason Origlieri ___________________________________________ A Dissertation Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES In Partial Fulfillment of the Requirements For the Degree of DOCTOR OF PHILOSOPHY In the Graduate College THE UNIVERSITY OF ARIZONA 2005 2 THE UNIVERSITY OF ARIZONA GRADUATE COLLEGE As members of the Dissertation Committee, we certify that we have read the dissertation prepared by Marcus Jason Origlieri entitled Crystal Chemistry of Selected Sb, As, and P Minerals and recommend that it be accepted as fulfilling the dissertation requirement for the Degree of Doctor of Philosophy _______________________________________________________________________ Date: November 15, 2005 Robert T. Downs _______________________________________________________________________ Date: November 15, 2005 M. Bonner Denton _______________________________________________________________________ Date: November 15, 2005 Mihai N. Ducea _______________________________________________________________________ Date: November 15, 2005 Charles T. Prewitt Final approval and acceptance of this dissertation is contingent upon the candidate’s submission of the final copies of the dissertation to the Graduate College. I hereby certify that I have read this dissertation prepared under my direction and recommend that it be accepted as fulfilling the dissertation requirement.
    [Show full text]
  • Mineral Processing
    Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19
    [Show full text]
  • Holdawayite Mn (CO3)
    2+ Holdawayite Mn6 (CO3)2(OH)7(Cl, OH) c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. Fibrous along [001]; commonly in granular aggregates, or massive, with individual grains to 2 cm. Physical Properties: Cleavage: On {100}, perfect. Fracture: Irregular. Tenacity: Moderately brittle. Hardness = ∼3 D(meas.) = 3.19(4) D(calc.) = 3.24 Optical Properties: Transparent to translucent. Color: Pale to dark pink if fresh, turning brown on exposure, developing a dark sooty coating. Streak: Pale pink. Luster: Vitreous, silky in fibrous aggregates. Optical Class: Biaxial (–). Orientation: X = b; Z ∧ c = 45(3)◦. Dispersion: r< v,moderate. α = 1.644(1) β = 1.719(1) γ = 1.721(1) 2V(meas.) = 12(3)◦ 2V(calc.) = 18◦ Cell Data: Space Group: C2/m. a = 23.437(5) b = 3.3137(3) c = 16.618(6) β = 111.15(2)◦ Z=4 X-ray Powder Pattern: Kombat mine, Namibia. 10.93 (100), 5.459 (80), 3.879 (70), 2.690 (60b), 2.589 (50b), 7.77 (40), 2.926 (40) Chemistry: (1) CO2 14.2 B2O3 1.2 FeO 0.2 MnO 64.6 MgO 4.4 CaO 0.5 Cl 4.4 H2O 11.47 −O=Cl2 1.0 Total 100.0 (1) Kombat mine, Namibia; by electron microprobe, C by Leco analyzer, H2O by the Penfield method, B may be due to sussexite contamination; corresponds to (Mn5.24Mg0.62 Ca0.06Fe0.02)Σ=5.94[(CO3)1.86(BO3)0.20]Σ=2.06[(OH)7.34Cl0.74]Σ=8.08. Occurrence: Locally abundant as a rare vein mineral in low-grade metamorphosed Mn-rich sedimentary rocks intercalated with sedimentary iron deposits.
    [Show full text]
  • Abstract Volume & Fieldtrip Guidebook
    SGA Student Conference Mineral resources for the society Prague, April 15‐19, 2011 Society for Geology Applied to Mineral Deposits & Charles University in Prague, Czech Republic SGA Student Conference Mineral resources for the society Prague, April 15‐19, 2011 ABSTRACT VOLUME & FIELD TRIP GUIDEBOOK Editor Kateřina Schlöglová 1 SGA Student Conference Mineral resources for the society Prague, April 15‐19, 2011 Contents Program of the conference 4 Abstract Volume Hydrotermal Alteration and Mass Change Calculations at the Mastra Au‐Ag Deposit, 8 Gümüşhane, Turkey Neslihan ASLAN & Miğraç AKÇAY Qualitative and quantitative analysis of talc from Western Carpathians 9 Vladimír ČAVAJDA, Peter UHLÍK & Ľubica PUŠKELOVÁ The Kombat Deposit in Namibia: A possible IOCG deposit 10 Nikola DENISOVÁ Geology and mineralization of the polymetallic Salt River deposit near Pofadder, 11 Namaqualand metamorphic province, South Africa Thomas DITTRICH, Bernhard SCHULZ, Jens GUTZMER, Keith OSBURN & Craig R. McCLUNG Application and significance of Vickers Microhardness Measurments for coal 12 Anne ENGLER Reactive fluid flow and origin of the fracture‐controlled greisens in the Krušné hory Mts., 13 Czech Republic Matylda HEŘMANSKÁ & David DOLEJŠ Low‐temperature alteration of metamict Y, REE, Nb, Ta, Ti oxide minerals 14 Nikola HEROLDOVÁ & Radek ŠKODA Grade and tonnage model for orogenic gold deposits in Finland and comparison with 15 Swedish, Zimbabwean, and Australian Southern Cross deposits Janne HOKKA Alteration styles and geochemical zonation at the Raitevarri
    [Show full text]
  • List of New Mineral Names: with an Index of Authors
    415 A (fifth) list of new mineral names: with an index of authors. 1 By L. J. S~v.scs~, M.A., F.G.S. Assistant in the ~Iineral Department of the,Brltish Museum. [Communicated June 7, 1910.] Aglaurito. R. Handmann, 1907. Zeita. Min. Geol. Stuttgart, col. i, p. 78. Orthoc]ase-felspar with a fine blue reflection forming a constituent of quartz-porphyry (Aglauritporphyr) from Teplitz, Bohemia. Named from ~,Xavpo~ ---- ~Xa&, bright. Alaito. K. A. ~Yenadkevi~, 1909. BuU. Acad. Sci. Saint-P6tersbourg, ser. 6, col. iii, p. 185 (A~am~s). Hydrate~l vanadic oxide, V205. H~O, forming blood=red, mossy growths with silky lustre. Founi] with turanite (q. v.) in thct neighbourhood of the Alai Mountains, Russian Central Asia. Alamosite. C. Palaehe and H. E. Merwin, 1909. Amer. Journ. Sci., ser. 4, col. xxvii, p. 899; Zeits. Kryst. Min., col. xlvi, p. 518. Lead recta-silicate, PbSiOs, occurring as snow-white, radially fibrous masses. Crystals are monoclinic, though apparently not isom0rphous with wol]astonite. From Alamos, Sonora, Mexico. Prepared artificially by S. Hilpert and P. Weiller, Ber. Deutsch. Chem. Ges., 1909, col. xlii, p. 2969. Aloisiite. L. Colomba, 1908. Rend. B. Accad. Lincei, Roma, set. 5, col. xvii, sere. 2, p. 233. A hydrated sub-silicate of calcium, ferrous iron, magnesium, sodium, and hydrogen, (R pp, R',), SiO,, occurring in an amorphous condition, intimately mixed with oalcinm carbonate, in a palagonite-tuff at Fort Portal, Uganda. Named in honour of H.R.H. Prince Luigi Amedeo of Savoy, Duke of Abruzzi. Aloisius or Aloysius is a Latin form of Luigi or I~ewis.
    [Show full text]
  • The Secondary Phosphate Minerals from Conselheiro Pena Pegmatite District (Minas Gerais, Brazil): Substitutions of Triphylite and Montebrasite Scholz, R.; Chaves, M
    The secondary phosphate minerals from Conselheiro Pena Pegmatite District (Minas Gerais, Brazil): substitutions of triphylite and montebrasite Scholz, R.; Chaves, M. L. S. C.; Belotti, F. M.; Filho, M. Cândido; Filho, L. Autor(es): A. D. Menezes; Silveira, C. Publicado por: Imprensa da Universidade de Coimbra URL persistente: URI:http://hdl.handle.net/10316.2/31441 DOI: DOI:http://dx.doi.org/10.14195/978-989-26-0534-0_27 Accessed : 2-Oct-2021 20:21:49 A navegação consulta e descarregamento dos títulos inseridos nas Bibliotecas Digitais UC Digitalis, UC Pombalina e UC Impactum, pressupõem a aceitação plena e sem reservas dos Termos e Condições de Uso destas Bibliotecas Digitais, disponíveis em https://digitalis.uc.pt/pt-pt/termos. Conforme exposto nos referidos Termos e Condições de Uso, o descarregamento de títulos de acesso restrito requer uma licença válida de autorização devendo o utilizador aceder ao(s) documento(s) a partir de um endereço de IP da instituição detentora da supramencionada licença. Ao utilizador é apenas permitido o descarregamento para uso pessoal, pelo que o emprego do(s) título(s) descarregado(s) para outro fim, designadamente comercial, carece de autorização do respetivo autor ou editor da obra. Na medida em que todas as obras da UC Digitalis se encontram protegidas pelo Código do Direito de Autor e Direitos Conexos e demais legislação aplicável, toda a cópia, parcial ou total, deste documento, nos casos em que é legalmente admitida, deverá conter ou fazer-se acompanhar por este aviso. pombalina.uc.pt digitalis.uc.pt 9 789892 605111 Série Documentos A presente obra reúne um conjunto de contribuições apresentadas no I Congresso Imprensa da Universidade de Coimbra Internacional de Geociências na CPLP, que decorreu de 14 a 16 de maio de 2012 no Coimbra University Press Auditório da Reitoria da Universidade de Coimbra.
    [Show full text]
  • Mineralogy and Metallogenesis of the Sanbao Mn–Ag (Zn-Pb) Deposit in the Laojunshan Ore District, SE Yunnan Province, China
    minerals Article Mineralogy and Metallogenesis of the Sanbao Mn–Ag (Zn-Pb) Deposit in the Laojunshan Ore District, SE Yunnan Province, China Shengjiang Du 1,2, Hanjie Wen 3,4,*, Shirong Liu 3, Chaojian Qin 3, Yongfeng Yan 5, Guangshu Yang 5 and Pengyu Feng 5 1 State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China; [email protected] 2 Chinese Academy of Geological Science, Beijing 100037, China 3 State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China; [email protected] (S.L.); [email protected] (C.Q.) 4 University of Chinese Academy of Sciences, Beijing 100049, China 5 Kunming University of Science and Technology, Kunming 650093, China; [email protected] (Y.Y.); [email protected] (G.Y.); [email protected] (P.F.) * Correspondence: [email protected] Received: 26 June 2020; Accepted: 17 July 2020; Published: 23 July 2020 Abstract: The Sanbao Mn–Ag (Zn-Pb) deposit located in the Laojunshan ore district is one of the most important deposits that has produced most Ag and Mn metals in southeastern Yunnan Province, China. Few studies are available concerning the distribution and mineralization of Ag, restricting further resource exploration. In this study, detailed mineralogy, chronology, and geochemistry are examined with the aim of revealing Ag occurrence and its associated primary base-metal and supergene mineralization. Results show that manganite and romanèchite are the major Ag-bearing minerals. Cassiterite from the Mn–Ag ores yielded a U–Pb age of 436 17 Ma, consistent with ± the Caledonian age of the Nanwenhe granitic pluton.
    [Show full text]
  • Download the Scanned
    INDEX,VOLUME 59* Absorption coefficients Albite, continued attapulgite 1113 1ow-, comparison with ussingite 347 clay ninerals 11r3 nelting in nultispecies fluid 598 dickite 274 Alexandrite, chrorniumIII centers in 159 hal loysite 274 hectorite I 113 ALLAN, DAVID illite 1113 with V. Brown, and J. Stark, Rocke kaolinite 274 and Minez,als of Califowi,a; reviewed metabentonite 1113 by J. Murdoch 387 nontronite 1113 Allemontite, see stibarsen 1331 srnectite 1113 ALLMAN,MICHAEL Absorption spectra with D.F. Lawrence, Geological alexandrite, synthetic 159 Labonatony Techni.ques reviewed apophyllite 62I ; by F.H. Manley and W.R. Powers IL42 garnet 565 olivine 244 A1lophane rhodonite.. shocked t77 dehydration, DTA, infrared spectra 1094 Acmite, Ti-, phase relations of 536 Almandine Actinolite overgrowth by grossularite- spessartine 558 coexisting with hoinblende 529 in netamorphic rocks, optical Arnerican Crystallographic Association, properties 22 abstracts, Spring neeting,1974 1L27 Activity coefficients Amphiboles of coexisting pyroxenes 204 actinolite 2? 529 Al -Ca-anphibole ADMS, HERBERTG. 22 compositions 22 with L.H. Cohen, and W. Klenent, Jr.; coordination polyhedra M High-low quartz inversion : Thermal of site atons in I 083 analysis studies to 7 kbar I 099 hornblende L, 22, 529, 604 ADAMS,JOHN W. magnesioarfvedsonite (authigenic) 830 with T. Botinelly, W.N. Sharp, and refraction indices 22 K. Robinson; Murataite, a new richterite, Mg-Fe- 518 conplex oxide from E1 Paso County, AMSTUTZ,G.C. Colorado L72 with A.J. Bernard, Eds., )nes in Errata 640 Sediments; reviewed by P.B. Barton 881 Aenigmatite ANDERSEN,C.A. in volcanic conplex, composition, and X-ray data Micz,opnobeAnalysis; reviewed by A.E.
    [Show full text]
  • Sugilite in Manganese Silicate Rocks from the Hoskins Mine and Woods Mine, New South Wales, Australia
    Sugilite in manganese silicate rocks from the Hoskins mine and Woods mine, New South Wales, Australia Y. KAWACHI Geology Department, University of Otago, P.O.Box 56, Dunedin, New Zealand P. M. ASHLEY Department of Geology and Geophysics, University of New England, Armidale, NSW 2351, Australia D. VINCE 1A Ramsay Street, Essendon, Victoria 3040, Australia AND M. GOODWIN P.O.Bo• 314, Lightning Ridge, NSW 2834, Australia Abstract Sugilite relatively rich in manganese has been found at two new localities, the Hoskins and Woods mines in New South Wales, Australia. The occurrences are in manganese-rich silicate rocks of middle to upper greenschist facies (Hoskins mine) and hornblende hornfels facies (Woods mine). Coexisting minerals are members of the namansilite-aegirine and pectolite-serandite series, Mn-rich alkali amphiboles, alkali feldspar, braunite, rhodonite, tephroite, albite, microcline, norrishite, witherite, manganoan calcite, quartz, and several unidentified minerals. Woods mine sugilite is colour-zoned with pale mauve cores and colourless rims, whereas Hoskins mine sugilite is only weakly colour-zoned and pink to mauve. Within single samples, the chemical compositions of sugilite from both localities show wide ranges in A1 contents and less variable ranges of Fe and Mn, similar to trends in sugilite from other localities. The refractive indices and cell dimensions tend to show systematic increases progressing from Al-rich to Fe- Mn-rich. The formation of the sugilite is controlled by the high alkali (especially Li) and manganese contents of the country rock, reflected in the occurrences of coexisting high alkali- and manganese- bearing minerals, and by high fo2 conditions. KEYWORDS: sugilite, manganese silicate rocks, milarite group, New South Wales, Australia Introduction Na2K(Fe 3 +,Mn 3 +,Al)2Li3Sit2030.
    [Show full text]
  • Utahite, a New Mineral and Associated Copper Tellurates from the Centennial Eureka Mine, Tintic District, Juab County, Utah
    UTAHITE, A NEW MINERAL AND ASSOCIATED COPPER TELLURATES FROM THE CENTENNIAL EUREKA MINE, TINTIC DISTRICT, JUAB COUNTY, UTAH Andrew C. Roberts and John A. R. Stirling Geological Survey of Canada 601 Booth Street Ottawa, Ontario, Canada K IA OE8 Alan J. Criddle Martin C. Jensen Elizabeth A. Moffatt Department of Mineralogy 121-2855 Idlewild Drive Canadian Conservation Institute The Natural History Museum Reno, Nevada 89509 1030 Innes Road Cromwell Road Ottawa, Ontario, Canada K IA OM5 London, England SW7 5BD Wendell E. Wilson Mineralogical Record 4631 Paseo Tubutama Tucson, Arizona 85750 ABSTRACT Utahite, idealized as CusZn;(Te6+04JiOH)8·7Hp, is triclinic, fracture. Utahite is vitreous, brittle and nonfluorescent; hardness space-group choices P 1 or P 1, with refined unit-cell parameters (Mohs) 4-5; calculated density 5.33 gtcm' (for empirical formula), from powder data: a = 8.794(4), b = 9996(2), c = 5.660(2);\, a = 5.34 glcm' (for idealized formula). In polished section, utahite is 104.10(2)°, f3 = 90.07(5)°, y= 96.34(3YO, V = 479.4(3) ;\3, a:b:c = slightly bireflectant and nonpleochroic. 1n reflected plane-polar- 0.8798:1 :0.5662, Z = 1. The strongest five reflections in the X-ray ized light in air it is very pale brown, with ubiquitous pale emerald- powder pattern are (dA(f)(hkl)]: 9.638(100)(010); 8.736(50)(100); green internal reflections. The anisotropy is unknown because it is 4.841(100)(020); 2.747(60)(002); 2.600(45)(301, 311). The min- masked by the internal reflections. Averaged electron-microprobe eral is an extremely rare constituent on the dumps of the Centen- analyses yielded CuO = 25.76, ZnO = 15.81, Te03 = 45.47, H20 nial Eureka mine, Tintic district, Juab County, Utah, where it (by difference) {12.96], total = {100.00] weight %, corresponding occurs both as isolated 0.6-mm clusters of tightly bound aggre- to CU49;Zn29lTe6+04)39l0H)79s' 7.1H20, based on 0 = 31.
    [Show full text]