Summer 1998 Gems & Gemology
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Redalyc.Mineralogical Study of the La Hueca Cretaceous Iron-Manganese
Revista Mexicana de Ciencias Geológicas ISSN: 1026-8774 [email protected] Universidad Nacional Autónoma de México México Corona Esquivel, Rodolfo; Ortega Gutiérrez, Fernando; Reyes Salas, Margarita; Lozano Santacruz, Rufino; Miranda Gasca, Miguel Angel Mineralogical study of the La Hueca Cretaceous Iron-Manganese deposit, Michoacán, south-western Mexico Revista Mexicana de Ciencias Geológicas, vol. 17, núm. 2, 2000, pp. 142-151 Universidad Nacional Autónoma de México Querétaro, México Available in: http://www.redalyc.org/articulo.oa?id=57217206 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Revista Mexicana de Ciencias Geológicas, volumen 17, número 2, 143 2000, p. 143- 153 Universidad Nacional Autónoma de México, Instituto de Geología, México, D.F MINERALOGICAL STUDY OF THE LA HUECA CRETACEOUS IRON- MANGANESE DEPOSIT, MICHOACÁN, SOUTHWESTERN MEXICO Rodolfo Corona-Esquivel1, Fernando Ortega-Gutiérrez1, Margarita Reyes-Salas1, Rufino Lozano-Santacruz1, and Miguel Angel Miranda-Gasca2 ABSTRACT In this work we describe for the first time the mineralogy and very briefly the possible origin of a banded Fe-Mn deposit associated with a Cretaceous volcanosedimentary sequence of the southern Guerrero terrane, near the sulfide massive volcanogenic deposit of La Minita. The deposit is confined within a felsic tuff unit; about 10 meters thick where sampled for chemical analysis. Using XRF, EDS and XRD techniques, we found besides todorokite, cryptomelane, quartz, romanechite (psilomelane), birnessite, illite-muscovite, cristobalite, chlorite, barite, halloysite, woodruffite, nacrite or kaolinite, and possibly hollandite-ferrian, as well as an amorphous material and two unknown manganese phases. -
Rhodochrosite Gems Unstable Colouration of Padparadscha-Like
Volume 36 / No. 4 / 2018 Effect of Blue Fluorescence on the Colour Appearance of Diamonds Rhodochrosite Gems The Hope Diamond Unstable Colouration of in London Padparadscha-like Sapphires Volume 36 / No. 4 / 2018 Cover photo: Rhodochrosite is prized as both mineral specimens and faceted stones, which are represented here by ‘The Snail’ (5.5 × 8.6 cm, COLUMNS from N’Chwaning, South Africa) and a 40.14 ct square-cut gemstone from the Sweet Home mine, Colorado, USA. For more on rhodochrosite, see What’s New 275 the article on pp. 332–345 of this issue. Specimens courtesy of Bill Larson J-Smart | SciAps Handheld (Pala International/The Collector, Fallbrook, California, USA); photo by LIBS Unit | SYNTHdetect XL | Ben DeCamp. Bursztynisko, The Amber Magazine | CIBJO 2018 Special Reports | De Beers Diamond ARTICLES Insight Report 2018 | Diamonds — Source to Use 2018 The Effect of Blue Fluorescence on the Colour 298 Proceedings | Gem Testing Appearance of Round-Brilliant-Cut Diamonds Laboratory (Jaipur, India) By Marleen Bouman, Ans Anthonis, John Chapman, Newsletter | IMA List of Gem Stefan Smans and Katrien De Corte Materials Updated | Journal of Jewellery Research | ‘The Curse Out of the Blue: The Hope Diamond in London 316 of the Hope Diamond’ Podcast | By Jack M. Ogden New Diamond Museum in Antwerp Rhodochrosite Gems: Properties and Provenance 332 278 By J. C. (Hanco) Zwaan, Regina Mertz-Kraus, Nathan D. Renfro, Shane F. McClure and Brendan M. Laurs Unstable Colouration of Padparadscha-like Sapphires 346 By Michael S. Krzemnicki, Alexander Klumb and Judith Braun 323 333 © DIVA, Antwerp Home of Diamonds Gem Notes 280 W. -
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. -
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 -
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. -
An Improved Approach to Crystal Symmetry and the Derivation And
71-22,530 SHANKLIN, Robert Elstone, 1915- AN IMPROVED APPROACH TO CRYSTAL SYMMETRY AND THE DERIVATION AND DESCRIPTION OF THE THIRTY- TWO CRYSTAL CLASSES BY MEANS OF THE STEREOGRAPHIC PROJECTION AND GROUP THEORY. The Ohio State University, Ph.D., 1971 Mineralogy University Microfilms, A XEROX Company , Ann Arbor, Michigan ©Copyright by Robert Elstone Shanklin 1971 AN IMPROVED APPROACH TO CRYSTAL SYMMETRY AND THE DERIVATION AND DESCRIPTION OF THE THIRTY-TNO CRYSTAL CLASSES BY MEANS OF THE STEREOGRA.PHIC PROJECTION AND GROUP THEORY DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Robert Elstone Shanklin, A. B., M.S ★ * * * * Approved By Department of Mineralogy PLEASE NOTE: Some pages have indistinct print. Filmed as received. UNIVERSITY MICROFILMS. PREFACE The subject of order in the natural world is a favorite topic of scientists and philosophers alike. If there is any order in the universe, the crystalline state seems to be an excellent place to find it. That which is orderly should be comprehensible. There is no reason why a subject as rich in educational value, as reward ing in intellectual content, and as full of aesthetic satisfaction as crystallography should remain behind a veil of obscurity, the property of a few specialists. As a teacher of crystallography and mineralogy for many years, it has become apparent to me that existing textbooks often do not serve the needs of either students or instructors. The material generally available on elementary crystallography seems to vary between excessively abstruse and involved on the one hand, or too brief on the other. -
108. the Crystal Structure O F Axinite Revised
490 Proc. Japan Acad., 45 (1969) [Vol. 45, 108. The Crystal Structure o f Axinite Revised By Tei-ichi ITO, M.J.A., Yoshio TAKEUCHI,*' Toru OzAWA,*' Takaharu ARAKI,**',fi' Tibor ZOLTAI,**' and J. J. FINNNEY***' (Comm. June 10, 1969) The crystal structure of axinite, H (Fe, Mn) Ca2A12BSi4016, was investigated by Ito and Takeuchi (1952) on the assumption that boron atoms in the structure form separate B03 groups like tourma- line (Ito, 1950; Ito and Sadanaga, 1951; vide Buerger et al., 1962). The structure then deduced by taking account of Patterson projec- tions consists of separate Si4012 and B03 groups bound together by Fe, Al and Ca atoms. Although the structure was crystallo-chemically reasonable, the residual R could not be reduced to less than 0.35 for all the reflections observed. Since axinite is one of those common silicate minerals whose crystal structure has not been refined, it has been thoroughly reinvestigated using modern techniques. The specimens used are from Woodlake, California (Type collec- tion #9620, Colorado School of Mines). Chemical analysis by an electron microprobe gives the Fe to Mn ratio of the specimen to be approximately unity. The lattice constants of the triclinic crystal are a=7.1566+0.0015, a=91.75°+0.83 b=9.1995±0.0020, 9=98.14° + 0.02 c=8.9585±0.0022, T=77.30° + 0.02 and the unit cell contains two formula units. Three dimensional intensities were collected by a scintillation counter using an equi- inclination single-crystal diffractometer, MoKa radiation and a pair of balanced Zr-Y filters. -
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. -
Compositional Characteristics of Kinoshitatite from the Sausar Group
American Mineralogist, Volume 74, pages 200-202, 1989 Compositionalcharacteristics of kinoshitatite from the SausarGroup, India SoNrN,q.rHD,c.scuprA., Slun Crr,cxRAnonrr, Puul.r SnNcurra, P. K. BnarrAcHARyA! H. BlNrn"rnn Centre of Advanced Study in Economic Geology, Department of Geological Sciences,Jadavpur University, Calcutta-700 032, India M. Furuoxe Department of Geology, Kyushu University, Fukuoka, Japan Anstnlcr Ba-rich and Ba-poor micas with varying Mn and Mg content in octahedralsites coexist in isolated pockets in braunite-bixbyite-hausmanniteores that have been invaded by late silicic pegmatite and carbonateveins in the SausarGroup, India. The micas are secondary in nature and are pseudomorphsafter carbonatesand alkali feldspars.One of the micas approachesclosely synthetic end-memberkinoshitalite, BaMgrAlrSirO,o(OH)..The present study shows a complete solid solution between the K (phlogopite) and Ba (kinoshitalite) end-members.Compositional diversities in these micas are attributable to the different minerals that the micas replaced. INlnolucrroN lites. Micas havedeveloped in manganeseoxide-rich rocks Krnoshitalite, BaMg.AlrSirOr0(OH)r, was defined by wherethe latter have beeninvaded by late silicic pegmatite Yoshii et al. (1973a)as the Ba and Mg trioctahedralbrit- and carbonateveins. In thesepockets, the manganeseox- tle mica. As an end-member, it is known only as a syn- ide-rich rocks exhibit the following mineral assemblage: thetic phase obtained hydrothermally at 600 "C and 2 braunite * hausmannite + bixbyite * Ba-bearingmica kbar (Frondel and Ito, 1967). Naturally occurring ki- + alkali feldspar + hematite * calcite + dolomite + noshitalite has been reported with considerableamounts qtrartz. The oxides collectively account for over 800/oof of K and Mn (Yoshii et al., l9l3b; Yoshii and Maeda, the rock. -
Manganese Deposits of Western Utah
Manganese Deposits of Western Utah GEOLOGICAL SURVEY BULLETIN 979-A Manganese Deposits of Western Utah By MAX D. CRITTENDEN, JR. , MANGANESE DEPOSITS OF UTAH, PART 1 GEOLOGICAL SURVEY BULLETIN 979-A A report on known deposits west of the lllth meridian * UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 19S1 UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price 50 cents (paper cover) CONTENTS Fag* Abstract.__________________________________________________________ 1 Introduction._._____.__________----_______-______-_--_------.__-__ 1 History of mining and production__.._______.______.___.__-___-_____ 2 Occurrence and age of the deposits_________-_____-_.-__-__-_-__--_- 6 Mineralogy _--____._____---_--_---_------------------------------- 7 Descriptions of the manganese minerals....____.__--_____-__-..__ 8 Oxides...___-__.--_--------___-_-_.-- . _ 8 Carbonates.___-____.__-____________-_-___-----_--------__ 9 Silicate.,_ _____-----_____--__-_______-_---___-__--___._--. 9 Relative stability and manganese content______--_----------_----_ 10 Oxidation and enrichment._____________________________________ 10 Classification and origin of the deposits....______.__._____---.___.-_-_ 11 General discussion_____________________________________________ 11 Syngenetic deposits_-_--____-----_--------------_-------__-_-.- 13 Bedded depositS-__________-_____._____..__________________ 13 Spring -
The Journal of Gemmology Editor: Dr R.R
he Journa TGemmolog Volume 25 No. 8 October 1997 The Gemmological Association and Gem Testing Laboratory of Great Britain Gemmological Association and Gem Testing Laboratory of Great Britain 27 Greville Street, London Eel N SSU Tel: 0171 404 1134 Fax: 0171 404 8843 e-mail: [email protected] Website: www.gagtl.ac.uklgagtl President: Professor R.A. Howie Vice-Presidents: LM. Bruton, Af'. ram, D.C. Kent, R.K. Mitchell Honorary Fellows: R.A. Howie, R.T. Liddicoat Inr, K. Nassau Honorary Life Members: D.). Callaghan, LA. lobbins, H. Tillander Council of Management: C.R. Cavey, T.]. Davidson, N.W. Decks, R.R. Harding, I. Thomson, V.P. Watson Members' Council: Aj. Allnutt, P. Dwyer-Hickey, R. fuller, l. Greatwood. B. jackson, J. Kessler, j. Monnickendam, L. Music, l.B. Nelson, P.G. Read, R. Shepherd, C.H. VVinter Branch Chairmen: Midlands - C.M. Green, North West - I. Knight, Scottish - B. jackson Examiners: A.j. Allnutt, M.Sc., Ph.D., leA, S.M. Anderson, B.Se. (Hons), I-CA, L. Bartlett, 13.Se, .'vI.phil., I-G/\' DCi\, E.M. Bruton, FGA, DC/\, c.~. Cavey, FGA, S. Coelho, B.Se, I-G,\' DGt\, Prof. A.T. Collins, B.Sc, Ph.D, A.G. Good, FGA, f1GA, Cj.E. Halt B.Sc. (Hons), FGr\, G.M. Howe, FG,'\, oo-, G.H. jones, B.Se, PhD., FCA, M. Newton, B.Se, D.PhiL, H.L. Plumb, B.Sc., ICA, DCA, R.D. Ross, B.5e, I-GA, DGA, P..A.. Sadler, 13.5c., IGA, DCA, E. Stern, I'GA, DC/\, Prof. I. -
June 2008 'Tairus' Created Gems: “Part I - Beryl”
Sponsored by Ministry of Commerce & Industry Volume 51 Lab Information Circular June 2008 'Tairus' Created Gems: “Part I - Beryl” In the Volume 49 of Lab Information Circular, November 2007, PleochroismPleochroism: : Dichroism varied from weak in aquamarine to we reported “Synthetic Beryl of Paraiba colour” produced by very strong in darker coloured varieties like purple pink or Tairus Co. Ltd. in order to take the advantage of the popularity of orange red (see figure 2). 'Paraiba' tourmalines. Thereafter, we procured sets of various coloured beryls and corundum from the same manufacturer for our research and reference purpose. The study of these sets has been divided into two parts; this issue describes the study of beryl set, while the study of corundum set will be published in the next issue. 2.a 2.c 2.e The Beryl set consisted of five colour varieties (figure 1), namely, green (emerald), light blue (aquamarine), electric greenish blue (paraiba type), purple pink and orange red. All specimens were facetted as square step and measured 6 X 6 mm. 2.b 2.d 2.f Figure 2 Pleochroic colours of Tairus created Beryls Absorption Spectrum:Spectrum : The spectrum varied as per the colour variety; emerald showed a typical chromium spectrum while 'paraiba' colour displayed a strong band at around 430 nm. Purple pink and orange red varieties exhibited strong bands at 460 to 490 and 550 to 600 nm. UV fluorescence:fluorescence : All samples were inert to long wave as well as short wave UV light. Figure 1 Chelsea Filter Reactioneaction: : Emerald revealed a red glow while all Standard gemmological tests and advanced analysis on FTIR other varieties were either inert or did not displayed any reaction.