Book Reviews 183

Total Page:16

File Type:pdf, Size:1020Kb

Book Reviews 183 Canadian Minerologist Vol.28, pp. 181-184(1990) BOOKREVIEWS Monteregian Treasur*, the Minerals of Mont Saint- systems.Appendix B givesX-ray powdo-diffragtion Hilaire, Quebec. By J. A. Mandarino and V. data in two separatesections: as an alphabetical spe- Anderson. Cambridge University Press,New York, cies list with the six strongest reflections, and as a 1989,281 pages,U.S.$85.fr). search index patterned after the Hanawalt method In less than thirty years Mont Saint-Hilaire, of JCPDS. Appendix C tabulates the species Quebec has emerged as one of the world's most accordingto tle ten geologicalenvironments outlined imFortant mineral localities. Over 2Z) confirmed spe- in Part one, Appendix D is a Dana classification of cies have been found to date, 15 of which are new the observed species,and Appendix E contains an to science,and a long list of unknowns still awaits exhaustivecompilation of chemicalanalyses of Mont further investigation. The majority of theseminerals Saint-Hilaire minerals presented in 4l tables occur in well-developed crystals and are eagerly according to chemical class.A comprehensivelist of sought by collectors from the amateur and profes- referencesis given in Part four. sional communitis alike. Large, high-quality crystals The text is clearly written throughout and can be ofsuch exotic speciesas leifite, carletonite, serand- read with easeby both professionals and educated ite, catapleiite,petarasite, and numerousothers have amateurs. Though not intended to be a comprehen- not been found elsewhere. sive petrological treatise, the sestion on the geology Monteregj an Treasuresis the first comprehensive ofthe occurrenceis disappointingly brief. There are work to deal with the mineralogy of Mont Saint- no geologicalor location maps given for the localiry. Hilaire. The text is divided into four parts. Part one $imilarly, the parageneticorganization of species presentsan abbreviated history of the evolution of according to their modes of ocqurence is both Mont Saint-Hilaire as a significant mineral locality desirableand instructive, but could have beenmuch and cratefully acknowledgestle role of the amateur more informative if developed further. A number in its development.A brief discussionof the geology of pageshave noticeable blank spaces,which some and petrology of the ocsurrence identifies ten geo- readersmay find objectionable, though others will logical environments of mineralogical interest: peg- probably welcomethis spaceto add their own notes matites, altered pegmatites,sodalite syenite, silicate- and new information as it becomesavailable. Simi- dominant cavities in nepheline syenite, carbonate- larly, opinions will probably be divided on the deci- dominant cavities in nepheline syenite, igneous sion to use only photomicrographs to illustrate breccia cavities, hornfels, marble xenoliths, sodalite specimensknown to exist plentifully as much larger xenoliths and rock-forming minslals. The distribu- specimens;but neither is that of seriousconsequence, tions of minerals among shemical classes,of chem- as Violet Anderson has done an admirable job in ical classesamong envirornents and of chemicalele- accurately rendering each speciesphotographed' an ments among environments also are considered. extremely difficult task consldering the subject size Part two constitutes the bulk of the text and pro- and technical limitations imposed by photomicrog- vides descriptiveand illustrative information for 221 raphy. Lastly, it would have been helpful to those species.Individual descriptionsare presentedalpha- readerswho may lack a firm understanding of crys- betically by speciesor group and include introduc- talloeraphy if the forms describedin the figure cap- tory remarks, notes on app€arance,physical proper- tions were also labeled on the crystal drawings. ties, occurrence and associated minerals, optical Regardless of any minor shortcomings, Mon- properties, chemical data, crystallography, distin- teregian Treasuresis a comprehensive, up-to-date gurshing features and other data. Computer- descriptive mineralogical text that successfully generatedcrystal drawings, photomicrographs(both bridgesthe gap betweenthe amateurand professional color and black and white) by Violet Anderson and minssal6gisl, and is certain to remain the definitive sketchesby Robert Fisher and Garry Glenn provide work on this classicminelnl locality for a long time a pleasing visual impast and illustrate well the spe- to come. Though moderately expensiveat U.S. cies they depict. $85.00, it wil be worth every p€nny to all serious Part tlree consistsof five useful appendicesthat collectors and professionals interestedin the miner- will be invaluable to those who routinely work with alogy of Mont Saint-Hilaire or alkali syenite com- Mont Saint-Hilaire minerals. Appendix A consists plexes in general. of an alphabetical tabulation of speciesby crystal GeorgeW. Robinson system and determinative tables arranged by axial National Museum of Natural Sciences ratios @onnay tables) for each of the six crystal Ottawa 18r r82 THE CANADIAN MINERALOGIST Introduction to Crystal Chemistry gtudent edition). reasonalone, the professionalwould probably prefer By H.W. Jaffe. CambridgeUniversity Press,Cam- to buy the completemonograph volume. bridge, 1988, 161 pages,f,9.00 (soft-bound only). Lee A. Groat This studentedition is Part I (Chapters l-ll: prin- The University of British Columbia ciples of Crystal Chemistry and Refractivity) of a larger two-part monograph volume, Crystal Chemistry and Refractivity (reviewed rn Con. Mineral. 14, 535). Part II of the larger volume is Mineralization and Shear Zones. Edited by J.T. titlercDecriptive Crystal Chemistry. T:hestudent edi- Bursnall. Short CourseVolume 6, GeologicalAssoci- tion is softbound, witl a cover illustration by M.C. ation of Canada, Department of Earth Sciences, Escher ("Stars"). University of Newfoundland, St. John's, Newfound- The book begins with a comprehensivereview of land AIB 3X5, 1988,?29 + rti pages.$25.@ for atomic structure and the periodic table, followed by membersof GAC; $35.00for nonmembers(ISBN a chapter on spectra, ionization potential, elec- 0-9t92t6-39-0\. tronegativity, and chemical bonding. Chapters 3-5 deal wilh Pauling's rules and the chemistry of cova- Owing the economic significance of Archean vein lent and ionic bonds. Chapter 6 looks at external gold deposits,a large number of symposia,confer- (nontranslational) and internal (translational) sym- ences,and short courseshave held over the last few metry. Chapter 7 servesas a short introduction ro years to ex?mine aspects of the geology and crystal-field theory. The next two chapters(8-9) deal geochemistryof thesedeposits. This volume is the with polyhedral distortion, diadochy, and isostruc- product ofone such short course,held in conjunc- tural crystals.Density, volume, unit cellsand packing tion with the 1989GAC-MAC national convention are consideredin Chapter 10. The book concludes and focussingon the structural and geochemicalrela- with an excellent introduction to refractivity and tions of Au mineralizationto shearzones. In view polarizability, in which both tle Lorentz-Lorenz and of the close genetic link between the evolution of Gladstone-Dale relationships are described; these shear zones and the formation of vein mineraliza- topics are rarely mentioned in introductory text- tion, the material dealt with in this volume should books. Each chapter is followed by a summary and be of interdst to geologists from industry, govern- bibliocraphy, and there is a limited appendix of ment and universities,who are involved in the explo- crystal-structure diagrams. ration for or researchon vein lode-gold deposits. The illustrations consist of line drawings and The book basically coverstlree aspectsof the rela- black-and-white photographs of packing models. tions betweenshear zones and lode-gold minerali- Some of the line drawings are confusing; more zation: l) Structural geology of shear zotes, 2) descriptivefigure-captions would help. One diagram Geochemistry of fluids associatedwith shear zones @ig. 1.2) is labeled incorrectly; the d1, arrd d* and gold mineralization, and 3) Application of struc- orbitals should be defined as d4, arid do, respec- tural analysis to the understanding of gold miner- tively. The photographs are generally clear and alization in the Superior Province of Ontario and informative. Quebec. In someareas, this book is not up-to-date. A com- The first four chapters deat with reviews of the prehensivelisting of ionic radii endswith Whittaker principles of structural geology as applied to shear & Muntus (1970); there is no mention of the studies zones, and some of the implications to the genesis by Shannon& Prewitt (1969)and Shannon(1976). of mineralization. Chapter I "Review of Mechan- Zachariasen'searly (1963)paper on bond strengths icat Principles, Deformation Mechanismsand Shear is mentioned,but not Brown,s (1981)study of the Zone Rosks" coversthe basic conceptsofstress and bond-valencenethod. Theseomissions may limit the strain in relation to ttre formation of shearzones and book's usefulnessas a referencehandbook. much of the experimental and theoretical data on Introduction to Crystal Chemistry is an excellent which the concepts are based. In addition, the role introduction to the relationship between mineral of fluids in deformation and the controls on varia- optics and structual crystallography. It is suitable tions in the brittle-ductile behavior of rocks are sum- for advancedundergraduate and beginninggraduate
Recommended publications
  • Infrared and Raman Spectroscopic Characterization of the Silicateв
    Journal of Molecular Structure 1042 (2013) 1–7 Contents lists available at SciVerse ScienceDirect Journal of Molecular Structure journal homepage: www.elsevier.com/locate/molstruc Infrared and Raman spectroscopic characterization of the silicate–carbonate mineral carletonite – KNa4Ca4Si8O18(CO3)4(OH,F)ÁH2O ⇑ Ray L. Frost a, , Yunfei Xi a, Ricardo Scholz b, Andrés López a, Fernanda Maria Belotti c a School of Chemistry, Physics and Mechanical Engineering, Science and Engineering Faculty, Queensland University of Technology, GPO Box 2434, Brisbane, Queensland 4001, Australia b Geology Department, School of Mines, Federal University of Ouro Preto, Campus Morro do Cruzeiro, Ouro Preto, MG 35400-00, Brazil c Federal University of Itajubá, Campus Itabira, Itabira, MG 35903-087, Brazil article info abstract Article history: An assessment of the molecular structure of carletonite a rare phyllosilicate mineral with general chem- Received 28 February 2013 ical formula given as KNa4Ca4Si8O18(CO3)4(OH,F)ÁH2O has been undertaken using vibrational spectros- Received in revised form 19 March 2013 copy. Carletonite has a complex layered structure. Within one period of c, it contains a silicate layer of Accepted 19 March 2013 composition NaKSi O ÁH O, a carbonate layer of composition NaCO Á0.5H O and two carbonate layers Available online 26 March 2013 8 18 2 3 2 of composition NaCa2CO3(F,OH)0.5. À1 2À Raman bands are observed at 1066, 1075 and 1086 cm . Whether these bands are due to the CO m1 Keywords: 3 symmetric stretching mode or to an SiO stretching vibration is open to question. Carletonite Multiple bands are observed in the 300–800 cmÀ1 spectral region, making the attribution of these Carbonate Infrared bands difficult.
    [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]
  • Apophyllite-(Kf)
    December 2013 Mineral of the Month APOPHYLLITE-(KF) Apophyllite-(KF) is a complex mineral with the unusual tendency to “leaf apart” when heated. It is a favorite among collectors because of its extraordinary transparency, bright luster, well- developed crystal habits, and occurrence in composite specimens with various zeolite minerals. OVERVIEW PHYSICAL PROPERTIES Chemistry: KCa4Si8O20(F,OH)·8H20 Basic Hydrous Potassium Calcium Fluorosilicate (Basic Potassium Calcium Silicate Fluoride Hydrate), often containing some sodium and trace amounts of iron and nickel. Class: Silicates Subclass: Phyllosilicates (Sheet Silicates) Group: Apophyllite Crystal System: Tetragonal Crystal Habits: Usually well-formed, cube-like or tabular crystals with rectangular, longitudinally striated prisms, square cross sections, and steep, diamond-shaped, pyramidal termination faces; pseudo-cubic prisms usually have flat terminations with beveled, distinctly triangular corners; also granular, lamellar, and compact. Color: Usually colorless or white; sometimes pale shades of green; occasionally pale shades of yellow, red, blue, or violet. Luster: Vitreous to pearly on crystal faces, pearly on cleavage surfaces with occasional iridescence. Transparency: Transparent to translucent Streak: White Cleavage: Perfect in one direction Fracture: Uneven, brittle. Hardness: 4.5-5.0 Specific Gravity: 2.3-2.4 Luminescence: Often fluoresces pale yellow-green. Refractive Index: 1.535-1.537 Distinctive Features and Tests: Pseudo-cubic crystals with pearly luster on cleavage surfaces; longitudinal striations; and occurrence as a secondary mineral in association with various zeolite minerals. Laboratory analysis is necessary to differentiate apophyllite-(KF) from closely-related apophyllite-(KOH). Can be confused with such zeolite minerals as stilbite-Ca [hydrous calcium sodium potassium aluminum silicate, Ca0.5,K,Na)9(Al9Si27O72)·28H2O], which forms tabular, wheat-sheaf-like, monoclinic crystals.
    [Show full text]
  • 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.
    [Show full text]
  • General Index
    CAL – CAL GENERAL INDEX CACOXENITE United States Prospect quarry (rhombs to 3 cm) 25:189– Not verified from pegmatites; most id as strunzite Arizona 190p 4:119, 4:121 Campbell shaft, Bisbee 24:428n Unanderra quarry 19:393c Australia California Willy Wally Gully (spherulitic) 19:401 Queensland Golden Rule mine, Tuolumne County 18:63 Queensland Mt. Isa mine 19:479 Stanislaus mine, Calaveras County 13:396h Mt. Isa mine (some scepter) 19:479 South Australia Colorado South Australia Moonta mines 19:(412) Cresson mine, Teller County (1 cm crystals; Beltana mine: smithsonite after 22:454p; Brazil some poss. melonite after) 16:234–236d,c white rhombs to 1 cm 22:452 Minas Gerais Cripple Creek, Teller County 13:395–396p,d, Wallaroo mines 19:413 Conselheiro Pena (id as acicular beraunite) 13:399 Tasmania 24:385n San Juan Mountains 10:358n Renison mine 19:384 Ireland Oregon Victoria Ft. Lismeenagh, Shenagolden, County Limer- Last Chance mine, Baker County 13:398n Flinders area 19:456 ick 20:396 Wisconsin Hunter River valley, north of Sydney (“glen- Spain Rib Mountain, Marathon County (5 mm laths donite,” poss. after ikaite) 19:368p,h Horcajo mines, Ciudad Real (rosettes; crystals in quartz) 12:95 Jindevick quarry, Warregul (oriented on cal- to 1 cm) 25:22p, 25:25 CALCIO-ANCYLITE-(Ce), -(Nd) cite) 19:199, 19:200p Kennon Head, Phillip Island 19:456 Sweden Canada Phelans Bluff, Phillip Island 19:456 Leveäniemi iron mine, Norrbotten 20:345p, Québec 20:346, 22:(48) Phillip Island 19:456 Mt. St-Hilaire (calcio-ancylite-(Ce)) 21:295– Austria United States
    [Show full text]
  • Carbon Mineral Ecology: Predicting the Undiscovered Minerals of Carbon
    American Mineralogist, Volume 101, pages 889–906, 2016 Carbon mineral ecology: Predicting the undiscovered minerals of carbon ROBERT M. HAZEN1,*, DANIEL R. HUMMER1, GRETHE HYSTAD2, ROBERT T. DOWNS3, AND JOSHUA J. GOLDEN3 1Geophysical Laboratory, Carnegie Institution, 5251 Broad Branch Road NW, Washington, D.C. 20015, U.S.A. 2Department of Mathematics, Computer Science, and Statistics, Purdue University Calumet, Hammond, Indiana 46323, U.S.A. 3Department of Geosciences, University of Arizona, 1040 East 4th Street, Tucson, Arizona 85721-0077, U.S.A. ABSTRACT Studies in mineral ecology exploit mineralogical databases to document diversity-distribution rela- tionships of minerals—relationships that are integral to characterizing “Earth-like” planets. As carbon is the most crucial element to life on Earth, as well as one of the defining constituents of a planet’s near-surface mineralogy, we focus here on the diversity and distribution of carbon-bearing minerals. We applied a Large Number of Rare Events (LNRE) model to the 403 known minerals of carbon, using 82 922 mineral species/locality data tabulated in http://mindat.org (as of 1 January 2015). We find that all carbon-bearing minerals, as well as subsets containing C with O, H, Ca, or Na, conform to LNRE distributions. Our model predicts that at least 548 C minerals exist on Earth today, indicating that at least 145 carbon-bearing mineral species have yet to be discovered. Furthermore, by analyzing subsets of the most common additional elements in carbon-bearing minerals (i.e., 378 C + O species; 282 C + H species; 133 C + Ca species; and 100 C + Na species), we predict that approximately 129 of these missing carbon minerals contain oxygen, 118 contain hydrogen, 52 contain calcium, and more than 60 contain sodium.
    [Show full text]
  • AUTHOR INDEX to VOLUME 56 3-4 620 3-4 665 L-2 354 7-8 Ll47 3-4 628 5-6 888 9-10 1760 L-2 307 7-8 1208 7-8 1180 9-10 1617 Rr-12 2
    AUTHOR INDEX TO VOLUME 56 Albright, Jarnes N. Vaterite stability 3-4 620 Allen, Rhesa M., Jr. Memorial of Alfred Leonard Anderson; November 19, 3-4 665 1900-January 27, 1964 1-9 1))') Anderson, C. P. Refinement ofthe crystal structure ofapophyllite; I, X'ray diffraction and physical properties Anderson, Charles P. Refinement of the crystal structure of apophyllite [abstr.] l-2 354 Anthony, John W. The crystal structure of legrandite 7-8 ll47 Aoki, Ilideki Reactions of magnesium carbonates by direct x-ray diffraction under 3-4 628 hydrothermal conditions Appleman, Daniel E. Crystal chemistry of a lunar pigeonite 5-6 888 Aramaki, Shigeo. Hydrothermal determination of temperature and water pressure of 9-10 1760 the magma of Aira caldera, Japan Arern, Joel E. Chevkinite and perrierite; synthesis, crystal growth and polymorphism l-2 307 Bachinski, Sharon W. Rate of Al-Si ordering in sanidines from an ignimbrite cooling 7-8 1208 unit Bailey, S. W. Antiphase domain structure of the intermediate composition plagioclase 7-8 1180 feldspars Bancroft, G. M. Miissbauer spectra of minerals along the diopside-hedenbergite tie 9-10 1617 line Barber, D. J. Mounting methods for mineral grains to be examined by high resolution rr-12 2152 electron microscopy Barton, Paul B., Jr. Sub-solidus relations in the system PbS-CdS ll-12 2034 Barton, R., Jr. Refinement of the crystal structure of elbaite [abstr.] r-2 356 Bates, Thornas F, Presentation of the Roebling Medal of the Mineralogical Society 3-4 653 of America for 1970 to George W. Brindley Bates,Ihornas F. Memorial of Paul Dimitri Krynine; September 19, 19O2-September 3-4 690 12.
    [Show full text]
  • Written in Stone: Remembering Master Facetor Art Grant
    GEMOLOGY Written in Stone: Remembering Master Faceter Art Grant By Elise A. Skalwold f ever a person’s legacy could be said to be “written Fig. 1: Arthur Tracey Grant, Jr. 1925-2015 in stone” it may well be that of legendary gem (Photo courtesy of cutter, Arthur Tracey Grant, Jr. who passed away on Nancy Grant Pritchard) September 24, 2015, in Richmond, Kentucky at the age of 90 (Fig. 1). Even for those Iwho do not frequent the yearly Fig. 2: The Scovil, Robert Weldon, Michael shows and symposia of the mineral 3,965.35-carat blue J. Bainbridge and Chip Clark; and gem community, a visit to the fluorite known as the latter’s images appear in the “Big Blue” from the venerable Smithsonian Institution in Minerva #2 mine, Smithsonian’s publications and Washington D.C. is hardly complete Hardin County, on its website. It was through a Illinois resides in without wandering through the gem the Smithsonian’s photographer’s eye and in the and mineral collections housed course of gemological studies Fig.2A: A restored National Gem within its great halls. 1987 snapshot of Collection, a gift of that I first became aware of the Harold and Doris Awestruck visitors, young and old, Art at the Desert astounding skill of this lapidary Inn, Tucson, Arizona Dibble in 1992 (Photo can gaze upon some of the largest holding the fluorite by Tino Hammid. artist and of the beauty which Courtesy of Nancy and most magnificent gemstones in octahedron from he was capable of bringing forth which he cut the Big Grant Pritchard).
    [Show full text]
  • CARLETONITE, Knaacaasiaors(Coe)4(F,OH)'H2O, a NEW MINERAL from MOUNT ST
    THE AMERICAN MINERALOGIST. VOL. 56. NOVEMBER-DECEMBER. 1S71 CARLETONITE, KNaaCaaSiaOrs(COe)4(F,OH)'H2O, A NEW MINERAL FROM MOUNT ST. HILAIRE, QUEBEC G. Y. Cnao, Departmentof Geology,Caileton University, Ottawa, Canad,a AesrnA,cr Carletonite, KNarCarSisOrs(COa){(l',OH).HrO, occurs in thermally metamorphosed inclusions in the nepheline syenite at Mount St. Hilaire, Quebec. It is associated mainly with pectolite. albite, arfvedsonite, calcite, fluorite, and apophyllite The mineral is tetragonal, PL/mbm, with o:13.178+.003 A, ,:16.695+.004 A, c/a:L2669. The strongest X-ray powder diffraction lines and their relative intensities (visual), are: 8.353(100),4.t7t(100),4.053(50), 2.903(90),2.384(60). Z:4 Carletonite is pink to pale blue, with vitreous to pearly luster. E:4-4; on {OOt}. Density (meas.):2.45 g/cma, (calc.):2.426g/cms. Cleavage{001 } perfect, {tt0} good, fracture conchoidal.Optically uniaxial ( - ), o: 1.521+ 0.001, e: 1.517* 0.001, in Na light, for pink and blue varieties. The blue variety is weakly pleochroic with O: very pale blue and E : very pale pinkish brown. Analyses of pink and blue varieties gave, respectively, SiOz M.9,44.7, TiO2 tr., tr., AlzOa0.5,0.6, total Fe n.d., n.d., MgO 0.C9, C.13, CaO 19.92, 19.97, NazO 10.23, 10.64, KzO 3.28,3.31,COz -,15.2, F 0.70,0.73, HrO- 0.70,C.63, HzO+ -, 3.51, LOI 19.92,-, sum 100.24,99.42, - (O:F, 0.29,0.30:99.95,99.1270.
    [Show full text]
  • 1 Geological Association of Canada Mineralogical
    GEOLOGICAL ASSOCIATION OF CANADA MINERALOGICAL ASSOCIATION OF CANADA 2006 JOINT ANNUAL MEETING MONTRÉAL, QUÉBEC FIELD TRIP 4A : GUIDEBOOK MINERALOGY AND GEOLOGY OF THE POUDRETTE QUARRY, MONT SAINT-HILAIRE, QUÉBEC by Charles Normand (1) Peter Tarassoff (2) 1. Département des Sciences de la Terre et de l’Atmosphère, Université du Québec À Montréal, 201, avenue du Président-Kennedy, Montréal, Québec H3C 3P8 2. Redpath Museum, McGill University, 859 Sherbrooke Street West, Montréal, Québec H3A 2K6 1 INTRODUCTION The Poudrette quarry located in the East Hill suite of the Mont Saint-Hilaire alkaline complex is one of the world’s most prolific mineral localities, with a species list exceeding 365. No other locality in Canada, and very few in the world have produced as many species. With a current total of 50 type minerals, the quarry has also produced more new species than any other locality in Canada, and accounts for about 25 per cent of all new species discovered in Canada (Horváth 2003). Why has a single a single quarry with a surface area of only 13.5 hectares produced such a mineral diversity? The answer lies in its geology and its multiplicity of mineral environments. INTRODUCTION La carrière Poudrette, localisée dans la suite East Hill du complexe alcalin du Mont Saint-Hilaire, est l’une des localités minéralogiques les plus prolifiques au monde avec plus de 365 espèces identifiées. Nul autre site au Canada, et très peu ailleurs au monde, n’ont livré autant de minéraux différents. Son total de 50 minéraux type à ce jour place non seulement cette carrière au premier rang des sites canadiens pour la découverte de nouvelles espèces, mais représente environ 25% de toutes les nouvelles espèces découvertes au Canada (Horváth 2003).
    [Show full text]
  • 3-4 648 Subject Index to Volume 56 3-4 653 3-4 657 3-4 643 3-4 646 7-8 1495 3-4 670 3-4 674 3-4 687 3-4 698 3-4 706 3-4
    SUBJECTINDEX TO VOLUME 56 Alaska Machatschki, Felix Karl Ludwig Mineralogy (Zemann, Josef.) 3-4 698 Mauguin, Charles Yugawaralite, Chena Hot Springs '706 (Eberlein, G. Donald, et al) 9-10 1699 (Wyart, Jean.) 3-4 Aluminum Miller, William John Analysis (Murdoch, Joseph.) 3-4 710 Electron probe, techniques Runner, Joseph James (Desborough, George A., et al.) (Glenister, Brian F., et al) 3-4 716 tt-12 2t29 Stewart, Duncan, VII Associations (Henrickson, Eiler L.) 3-4 720 Mineralogical Society of America Walker, George Forbes Award, 1970, Evans, Bernard W., accept'ance (Brindley, G. W.) 3-4 728 (Evans, Bernard W.) 3-4 663 Europe Award, 1970, Evans, Bernard W., Germany, history of research,book presentation revlews (Fyfe, w. S.) 3-4 660 (Schmidt, Peter.) 7-8 1495 Roebling Medal, 1970, Brindley, George Biography W., presentation Anderson, Alfred Leonard (Bates, Thomas F.) 3-4 653 Roebling Medal, 1970, Brindley, George (Allen, 3-4 665 W., acceptance Rhesa M., Jr.) (Brindley, G. W.) 3-4 657 Barlett, Helen Blair Australia Bibliography Mineralogy (Schwartzwalder, Karl.) 3-4 669 Book reviews Bowles, Oliver (Chalmers, R. O.) 3-4 643 Bibliography Petrology (Josephson,G. W.) 3-4 670 Book reviews Currier, Louis ll/ade (Joplin, Germaine A.) 3-4 646 Bibliography Automatic data processing (Jahns, Richard H.) 3-4 674 Applications Foster, Margaret D. Petrology, mineralogy, book reviews Bibliography (Harrison, R. K., e/ a/.) 3-4 648 (Fahey, Joseph J.) 3-4 687 Bibliography Krynine, Paul Dimitri Authors Bibliography Barlett, Helen Blair (Bates, Thomas F., et aL\ 3-4 690 (Schwartzwalder, Karl.) 3-4 669 Machatschki, Felix Karl Ludwig Bowles, Oliver Bibliography (Josephson, G.
    [Show full text]
  • Twenty-Seventh List of New Mineral Names
    MINERALOGICAL MAGAZINE, DECEMBER 1972, VOL. 38, PP. 987-1OOl Twenty-seventh list of new mineral names M. H. HEY AND P. G. EMBREY Department of Mineralogy, British Museum (Natural History), London SW7 THE present list includes 147 names, of which 9 are spelling variants or errors, 26 new and unnecessary synonyms for known minerals and names for synthetic or hypo- thetical products not known in nature, and I4 a group of unnecessary varietal names proposed over a century ago by J. Frrbel, most of which have escaped inclusion in the literature until now, but are here noted 'for the record'. Names for inadequately characterized minerals 02) and names for minor varieties (I) still constitute an un- necessary burden on the literature. Most of the 85 new named species have been approved prior to publication by the Commission on New Minerals and Mineral Names of the International Mineralogical Association, and it is noticeable that few of those published without the Commission's approval are likely to prove worthy of species rank; in the present list names (other than spelling variants) published since I96o without the Commission's approval are distinguished by an asterisk (*); valid species are in bold-face type. To save space, references to certain journals are sometimes given in shortened form: A.M., Amer. Min. ; Bull., Bull. Soc. frang. Min. Crist. ; M.A., Mineralogical Abstracts; Zap., 3at1. Beecoto3. Mnn. o6~. (Mem. All-Union Min. Soe.). Agrinierite. F. Cesbron, W. L. Brown, P. Bariand, and J. Geffroy, 1972. Min. Mag. 38, 78I. Orange orthorhombi~ crystals, a 14"o4, b 24.o7, c 14.13 A, Cmmm, D 5"7, occur with uranophane in cavities in gummite at Margnac, France.
    [Show full text]