DOCSLIB.ORG

THE 6Th INTERNATIONAL SYMPOSIUM on GRANITIC PEGMATITES

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
THE 6Th INTERNATIONAL SYMPOSIUM on GRANITIC PEGMATITES CONTRIBUTIONS TO THE 6th INTERNATIONAL SYMPOSIUM ON GRANITIC PEGMATITES EDITORS WILLIAM B. SIMMONS KAREN L. WEBBER ALEXANDER U. FALSTER ENCARNACIÓN RODA-ROBLES SARAH L. HANSON MARÍA FLORENCIA MÁRQUEZ-ZAVALÍA MIGUEL ÁNGEL Galliski GUEST EDITORS ANDREW P. BOUDREAUX KIMBERLY T. CLARK MYLES M. FELCH KAREN L. MARCHAL LEAH R. GRASSI JON GUIDRY SUSANNA T. KREINIK C. MARK JOHNSON COVER DESIGN BY RAYMOND A. SPRAGUE PRINTED BY RUBELLITE PRESS, NEW ORLEANS, LA PEG 2013: The 6th International Symposium on Granitic Pegmatites PREFACE Phosphate Theme Session Dedicated to: François Fontan, André-Mathieu Fransolet and Paul Keller, It is a pleasure for the organizing committee to phosphates during the evolution of the pegmatites introduce the special session on phosphates, as an and on their relationship to other mineral phases, important part of the program of the 6th such as silicates. These kinds of studies are getting International Symposium on Granitic Pegmatites. more and more abundant, with some interesting The complexity of phosphate associations, examples in this volume. commonly occurring as a mixture of several fine- We take this opportunity to honor François grained phases, make their study difficult. However Fontan, Paul Keller and André-Mathieu Fransolet. over the last decades, the number of publications on These three exceptional researchers have pegmatite phosphate minerals has increased contributed enormously to the advancement in the exponentially as a result of new techniques. The knowledge on phosphates during the last decades. early investigations focused on description, They worked individually and jointly, always in an composition and paragenesis. Now that most of the enthusiastic, effective and tireless way. They passed phases have been extensively described and their knowledge and interest in phosphates onto replacement sequences of secondary phosphates are many younger researchers. Now we would like to better understood, we are at the beginning of a new thank them sincerely for all their work. frontier of investigations of the petrogenetic role of François Fontan was born in Toulouse (France) in 1942, and he passed away six years ago, in July 2007, at the age of 64. François spent his career in research with the CNRS, at the Université Paul-Sabatier in Toulouse (France). He obtained his Doctorat d’Etat in 1971, under the guidance of François Permingeat, a founder of the International Mineralogical Association. He was particularly involved in investigations of the mineralogy and genesis of phosphate minerals in granitic pegmatites. With other specialists, he worked on the characterization of complex assemblages of phosphates in pegmatites in several European and African countries. Among his list of more than one hundred articles are descriptions of eight new mineral species. Fontanite, (Ca[(UO2)3(CO3)2O2]•6(H2O)) was named in recognition of his accomplishments. PREFACE Page ii PEG 2013: The 6th International Symposium on Granitic Pegmatites André-Mathieu Fransolet was born in Heusy (Belgium) in May of 1947. He finished his studies in Geology at the Université de Liège in October of 1969. In 1975 he defended his PhD Thesis on Geological and Mineralogical Sciences, at the same university, where he also developed most of his fruitful research, until he retired last year. During that time he published more than one hundred papers, most of them on phosphates associated with pegmatites all over the world and he contributed to the discovery of ten new mineral species. There are two mineral phases named after him: Fransoletite (H2Ca3Be2(PO4)4•4(H2O)) and parafransoletite (Ca3Be2(PO4)2(PO3,OH)2•4(H2O)) Paul Keller was born in Sarata, Romania in 1940. He finished his studies in Crystal Chemistry of Phosphates and Arsenates at The University of Stuttgart (Germany), in 1973. He worked for many years at the Institut für Mineralogie und Kristallchemie, at the University of Stuttgart (Germany), where he retired in 2006. His research on phosphates was very broad, with the publication of more than one hundred scientific papers, including the discovery of close to a dozen new mineral species. The phosphate paulkellerite (Bi2Fe(PO4)O2(OH)2) was named after him, in recognition of his productive career. (photograph courtesy of Anthony Kampf). PREFACE Page iii PEG 2013: The 6th International Symposium on Granitic Pegmatites TABLE OF CONTENTS KEYNOTE SPEAKERS Crystal Chemistry and Geothermometric Applications of Primary Pegmatite Phosphates F. HATERT ........................................................................................................................................................................................... 1 Reading Pegmatites: What Minerals Say D. LONDON ........................................................................................................................................................................................... 5 The Late-Stage Mini-Flood of Ca in Granitic Pegmatites: A Working Hypothesis R. MARTIN ............................................................................................................................................................................................ 7 Productive “Zones” in Gem-Bearing Pegmatites of Central Madagascar, Geochemical Evolution and Genetic Inferences F. PEZZOTTA ........................................................................................................................................................................................ 9 CONTRIBUTIONS Pegmatitic Rocks in a Migmatite-Granite Complex (NW Portugal) M. AREIAS, M. RIBEIRO, A. DÓRIA ....................................................................................................................................................... 12 Unraveling the Fluid Evolution of Mineralized Pegmatites in Namibia L. ASHWORTH, J. KINNAIRD, P. NEX .................................................................................................................................................... 14 The Phosphate Minerals Assemblages from Jocão Pegmatite, Minas Gerais, Brazil M. BAIJOT, F. HATERT, S. PHILIPPO ..................................................................................................................................................... 16 Preliminary Crystallography and Spectroscopy Data of Euclase from Northeast of Brazil S. BARRETO, DE B., V. ZEBEC, A ČOBIĆ, R.WEGNER, R BRANDÃO, P. GUZZO, L. SANTOS, V. BEGIĆ, V. BERMANEC ............................. 18 Two Generations of Microcline from Mount Malosa Pegmatite, Zomba District, Malawi V. BERMANEC, M. HORVAT, Ž. ŽIGOVEČKI GOBAC, V. ZEBEC ............................................................................................................... 20 Chrysoberyl in Association with Sillimanite at Roncadeira in the Borborema Pegmatite Province, Northeastern Brazil: Petrogenetic and Gemological Implications H. BEURLEN, D. RHEDE, R. THOMAS, D. SOARES, M. DA SILVA ............................................................................................................ 22 Cartography to Chemistry: Estimating the Bulk Composition of the Mt Mica Pegmatite via Map Analysis, Maine, USA A. BOUDREAUX, L. GRASSI, W. SIMMONS, A. FALSTER, K. WEBBER, G. FREEMAN ................................................................................ 24 Accessory Mineralogy of an Evolved Pegmatite, Dickinson County, Michigan T. BUCHHOLZ, A. FALSTER , W. SIMMONS ............................................................................................................................................ 26 The Ponte Segade Deposit (Galicia, NW Spain): A Recently Discovered Occurrence of Rare-Element Pegmatites F. CANOSA, M. FUERTES-FUENTE, A. MARTIN-IZARD ........................................................................................................................... 28 Contact Zone Mineralogy and Geochemistry of Mount Mica Pegmatite, Oxford Co., Maine, USA K. CLARK, W. SIMMONS, K. WEBBER, A. FALSTER, E. RODA-ROBLES, G. FREEMAN.............................................................................. 30 Preliminary 57Fe Mössbauer Spectroscopy Study of Metamict Allanite-(Ce) from Granitic Pegmatite, Fone, Aust-Agder, Norway A.ČOBIĆ, C.MCCAMMON, N.TOMAŠIĆ, V.BERMANEC ........................................................................................................................... 32 2+ 2+ Crystal Chemistry of M Be2P2O8 (M = Ca, Sr, Pb, Ba) Beryllophosphates: A Comparison with Feldspar Analogues F. DAL BO, F. HATERT, C. RAO ........................................................................................................................................................... 34 Spatial Statistical Analysis Applied to Rare-Elements LCT-Type Pegmatite Fields: An Original Approach to Constrain Faults-Pegmatites-Granites Relationships S. DEVEAUD, C. GUMIAUX , E. GLOAGUEN, Y. BRANQUET .................................................................................................................... 36 Be and Zn Behavior During Anatetic Formation of Early Pegmatoid Melts in Variscan Terrains – An Example from the Arga Pegmatite Field, Northern Portugal P. DIAS, C. LEAL GOMES ..................................................................................................................................................................... 37 Structural and Paragenetic Analysis of Swarms of Bubble Like Pegmatites in a Miarolitic Granite from Assunção South – Viseu – Central Portugal P. A. DIAS, P. ARAÚJO, M. PEREIRA,
Load more

Recommended publications
  • 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.
    [Show full text]
  • Kosnarite Kzr2(PO4)3 C 2001-2005 Mineral Data Publishing, Version 1
    Kosnarite KZr2(PO4)3 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal, pseudocubic. Point Group: 32/m. As rhombohedral pseudocubic crystals, to 0.9 mm, with {1012} and tiny {0001}. Physical Properties: Cleavage: Perfect on {1012}. Fracture: Conchoidal. Tenacity: Brittle. Hardness = 4.5 D(meas.) = 3.194(2) D(calc.) = 3.206 Optical Properties: Transparent to translucent. Color: Pale blue to blue-green, bluish gray, nearly colorless. Streak: White. Luster: Vitreous. Optical Class: Uniaxial (+). ω = 1.656(2) = 1.682(2) Cell Data: Space Group: R3c. a = 8.687(2) c = 23.877(7) Z = 6 X-ray Powder Pattern: Mt. Mica, Maine, USA. 4.329 (100), 3.806 (90), 2.928 (90), 6.41 (50), 4.679 (50), 2.502 (50), 1.903 (45) Chemistry: (1) (2) (3) P2O5 43.3 42.2 42.04 ZrO2 44.5 47.9 48.66 HfO2 0.5 0.9 FeO 0.2 < 0.1 MnO 1.0 < 0.1 Na2O 1.4 < 0.1 K2O 8.7 9.25 9.30 Rb2O 0.25 0.2 F 0.20 0.2 −O=F2 0.08 0.08 Total 99.97 100.57 100.00 (1) Mt. Mica, Maine, USA; by electron microprobe, total Fe as FeO, total Mn as MnO; corresponds to (K0.93Na0.08Rb0.01)Σ=1.02(Zr1.81Na0.15Mn0.07Fe0.01Hf0.01)Σ=2.05 [P1.02(O3.98F0.02)Σ=4.00]3. (2) Black Mountain, Maine, USA; by electron microprobe, total Fe as FeO, total Mn as MnO; corresponds to (K0.99Rb0.01)Σ=1.00(Zr1.96Hf0.02)Σ=1.98 [P1.00(O3.98F0.02)Σ=4.00]3.
    [Show full text]
  • Ceramic Mineral Waste-Forms for Nuclear Waste Immobilization
    materials Review Ceramic Mineral Waste-Forms for Nuclear Waste Immobilization Albina I. Orlova 1 and Michael I. Ojovan 2,3,* 1 Lobachevsky State University of Nizhny Novgorod, 23 Gagarina av., 603950 Nizhny Novgorod, Russian Federation 2 Department of Radiochemistry, Lomonosov Moscow State University, Moscow 119991, Russia 3 Imperial College London, South Kensington Campus, Exhibition Road, London SW7 2AZ, UK * Correspondence: [email protected] Received: 31 May 2019; Accepted: 12 August 2019; Published: 19 August 2019 Abstract: Crystalline ceramics are intensively investigated as effective materials in various nuclear energy applications, such as inert matrix and accident tolerant fuels and nuclear waste immobilization. This paper presents an analysis of the current status of work in this field of material sciences. We have considered inorganic materials characterized by different structures, including simple oxides with fluorite structure, complex oxides (pyrochlore, murataite, zirconolite, perovskite, hollandite, garnet, crichtonite, freudenbergite, and P-pollucite), simple silicates (zircon/thorite/coffinite, titanite (sphen), britholite), framework silicates (zeolite, pollucite, nepheline /leucite, sodalite, cancrinite, micas structures), phosphates (monazite, xenotime, apatite, kosnarite (NZP), langbeinite, thorium phosphate diphosphate, struvite, meta-ankoleite), and aluminates with a magnetoplumbite structure. These materials can contain in their composition various cations in different combinations and ratios: Li–Cs, Tl, Ag, Be–Ba, Pb, Mn, Co, Ni, Cu, Cd, B, Al, Fe, Ga, Sc, Cr, V, Sb, Nb, Ta, La, Ce, rare-earth elements (REEs), Si, Ti, Zr, Hf, Sn, Bi, Nb, Th, U, Np, Pu, Am and Cm. They can be prepared in the form of powders, including nano-powders, as well as in form of monolith (bulk) ceramics.
    [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]
  • 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]
  • A Raman and Infrared Spectroscopic Analysis of the Phosphate Mineral
    Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy 126 (2014) 164–169 Contents lists available at ScienceDirect Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy journal homepage: www.elsevier.com/locate/saa A Raman and infrared spectroscopic analysis of the phosphate mineral wardite NaAl3(PO4)2(OH)4Á2(H2O) from Brazil ⇑ Ray L. Frost a, , Ricardo Scholz b, Andrés López a, Cristiano Lana b, Yunfei Xi a 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 highlights graphical abstract A wardite mineral sample from Lavra Da Ilha, Minas Gerais, Brazil was analysed. Using SEM with EDX and vibrational spectroscopy. The calculated formula is (Na0.97Ca0.03)R1.00Al3 (PO4)2(OH)4Á2(H2O). Observation of multiple bands supports the concept of non- equivalent phosphate units in the structure. article info abstract Article history: A wardite mineral sample from Lavra Da Ilha, Minas Gerais, Brazil has been examined by vibrational spec- Received 17 November 2013 troscopy. The mineral is unusual in that it belongs to a unique symmetry class, namely the tetragonal-tra- Received in revised form 7 January 2014 pezohedral group. The structure of wardite contains layers of corner-linked –OH bridged MO6 octahedra Accepted 2 February 2014 stacked along the tetragonal C-axis in a four-layer sequence and linked by PO groups. Consequentially Available online 15 February 2014 4 not all phosphate units are identical.
    [Show full text]
  • Tetrahedral Boron in Naturally Occurring Tourmaline LETTERS
    American Mineralogist, Volume 84, pages 1451–1455, 1999 LETTERS Tetrahedral boron in naturally occurring tourmaline S.L. TAGG,1,* HERMAN CHO,1,† M. DARBY DYAR,2 AND EDWARD S. GREW3 1Environmental Molecular Sciences Laboratory MS K8-98, Pacific Northwest National Laboratory, P.O. Box 999, Richland, Washington 99352, U.S.A. 2Department of Geology and Geography, Mount Holyoke College, South Hadley, Massachusetts 01075, U.S.A. 3Department of Geological Sciences, University of Maine, Orono, Maine 04469, U.S.A. ABSTRACT Evidence for boron in both trigonal and tetrahedral coordination has been found in 11B magic- angle-spinning (MAS) nuclear magnetic resonance (NMR) spectra of natural, inclusion-free speci- mens of aluminum-rich lithian tourmaline from granitic pegmatites. INTRODUCTION tent with some substitution of silicon by boron (Hawthorne Minerals of the tourmaline group are by far the most wide- 1996). Wodara and Schreyer (1997; 1998) synthesized olenites spread borosilicate phases and the dominant carriers of boron in with an even greater amount of excess boron and boron substi- 11 crustal metamorphic and igneous rocks. The amount of boron tution for silicon, and cited B magic-angle-spinning (MAS) and its crystallographic position in tourmaline are of interest not nuclear magnetic resonance (NMR) evidence for the presence only to mineralogists, but also to geochemists studying the be- of both trigonal and tetrahedral boron. In summary, the coor- havior of boron and its isotopes in natural systems. Previous dination and partitioning of boron in tourmaline have not yet studies of boron contents in tourmaline have yielded variable been definitively characterized. In part, this results from in- results.
    [Show full text]
  • 38Th RMS Program Notes
    E.fu\wsoil 'og PROGRAM Thursday Evening, April 14, 2011 PM 4:00-6:00 Cocktails and Snacks – Hospitality Suite 400 (4th Floor) 6:00-7:45 Dinner – Baxter’s 8:00-9:15 THE GUALTERONI COLLECTION: A TIME CAPSULE FROM A CENTURY AGO – Dr. Renato Pagano In 1950, the honorary curator of the Museum of Natural History in Genoa first introduced Dr. Renato Pagano to mineral collecting as a Boy Scout. He has never looked back. He holds a doctorate in electrical engineering and had a distinguished career as an Italian industrialist. His passion for minerals has produced a collection of more than 13,000 specimens, with both systematic and aesthetic subcollections. His wife Adriana shares his passion for minerals and is his partner in collecting and curating. An excellent profile of Renato, Adriana, and their many collections appeared earlier this year in Mineralogical Record (42:41-52). Tonight Dr. Pagano will talk about an historic mineral collection assembled between 1861 and 1908 and recently acquired intact by the Museum of Natural History of Milan. We most warmly welcome Dr. Renato Pagano back to the speakers’ podium. 9:15 Cocktails and snacks in the Hospitality Suite on the 4th floor will be available throughout the rest of the evening. Dealers’ rooms will be open at this time. All of the dealers are located on the 4th floor. Friday Morning, April 15, 2011 AM 9:00 Announcements 9:15-10:15 CRACKING THE CODE OF PHLOGOPITE DEPOSITS IN QUÉBEC (PARKER MINE), MADAGASCAR (AMPANDANDRAVA) AND RUSSIA (KOVDOR) – Dr. Robert F. Martin Robert François Martin is an emeritus professor of geology at McGill University in Montreal.
    [Show full text]
  • Rep 2 out Public 2010 S Tlet Sur of Ma Urvey Rvey Adagas Repor Scar Rt
    Evidence for Malaria Medicines Policy Outlet Survey Republic of Madagascar 2010 Survey Report MINSTERE DE LA SANTE PUBLIQUE www. ACTwatch.info Copyright © 2010 Population Services International (PSI). All rights reserved. Acknowledgements ACTwatch is funded by the Bill and Melinda Gates Foundation. This study was implemented by Population Services International (PSI). ACTwatch’s Advisory Committee: Mr. Suprotik Basu Advisor to the UN Secretary General's Special Envoy for Malaria Mr. Rik Bosman Supply Chain Expert, Former Senior Vice President, Unilever Ms. Renia Coghlan Global Access Associate Director, Medicines for Malaria Venture (MMV) Dr. Thom Eisele Assistant Professor, Tulane University Mr. Louis Da Gama Malaria Advocacy & Communications Director, Global Health Advocates Dr. Paul Lavani Executive Director, RaPID Pharmacovigilance Program Dr. Ramanan Senior Fellow, Resources for the Future Dr. Matthew Lynch Project Director, VOICES, Johns Hopkins University Centre for Dr. Bernard Nahlen Deputy Coordinator, President's Malaria Initiative (PMI) Dr. Jayesh M. Pandit Head, Pharmacovigilance Department, Pharmacy and Poisons Board‐Kenya Dr. Melanie Renshaw Advisor to the UN Secretary General's Special Envoy for Malaria Mr. Oliver Sabot Vice‐President, Vaccines Clinton Foundation Ms. Rima Shretta Senior Program Associate, Strengthening Pharmaceutical Systems Dr. Rick Steketee Science Director, Malaria Control and Evaluation Partnership in Africa Dr. Warren Stevens Health Economist Dr. Gladys Tetteh CDC Resident Advisor, President’s Malaria
    [Show full text]
  • 1469 Vol 43#5 Art 03.Indd
    1469 The Canadian Mineralogist Vol. 43, pp. 1469-1487 (2005) BORATE MINERALS OF THE PENOBSQUIS AND MILLSTREAM DEPOSITS, SOUTHERN NEW BRUNSWICK, CANADA JOEL D. GRICE§, ROBERT A. GAULT AND JERRY VAN VELTHUIZEN† Research Division, Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario K1P 6P4, Canada ABSTRACT The borate minerals found in two potash deposits, at Penobsquis and Millstream, Kings County, New Brunswick, are described in detail. These deposits are located in the Moncton Subbasin, which forms the eastern portion of the extensive Maritimes Basin. These marine evaporites consist of an early carbonate unit, followed by a sulfate, and fi nally, a salt unit. The borate assemblages occur in specifi c beds of halite and sylvite that were the last units to form in the evaporite sequence. Species identifi ed from drill-core sections include: boracite, brianroulstonite, chambersite, colemanite, congolite, danburite, hilgardite, howlite, hydroboracite, kurgantaite, penobsquisite, pringleite, ruitenbergite, strontioginorite, szaibélyite, trembathite, veatchite, volkovskite and walkerite. In addition, 41 non-borate species have been identifi ed, including magnesite, monohydrocalcite, sellaite, kieserite and fl uorite. The borate assemblages in the two deposits differ, and in each deposit, they vary stratigraphically. At Millstream, boracite is the most common borate in the sylvite + carnallite beds, with hilgardite in the lower halite strata. At Penobsquis, there is an upper unit of hilgardite + volkovskite + trembathite in halite and a lower unit of hydroboracite + volkov- skite + trembathite–congolite in halite–sylvite. At both deposits, values of the ratio of B isotopes [␦11B] range from 21.5 to 37.8‰ [21 analyses] and are consistent with a seawater source, without any need for a more exotic interpretation.
    [Show full text]
  • NVMC Nov 2019 Newsletter.Pdf
    The Mineral Newsletter Meeting: November 18 Time: 7:45 p.m. Long Branch Nature Center, 625 S. Carlin Springs Rd., Arlington, VA 22204 Volume 60, No. 9 November 2019 Explore our website! November Meeting Program: Making Sugarloaf Mountain (details on page 5) In this issue … Mineral of the month: Datolite ................. p. 2 November program details ........................ p. 5 Annual Holiday Party coming up! ............. p. 5 President’s collected thoughts .................. p. 5 October meeting minutes .......................... p. 7 Nominations for 2019 club officers ........... p. 8 Datolite nodule Club show volunteers needed! .................. p. 8 Quincy Mine, Michigan Bench tip: Sheet wax with adhesives ......... p. 9 Source: Brandes (2019). Photo: Paul T. Brandes. Annual show coming up—Help needed! .. p. 10 EFMLS: Wildacres—finally! ........................ p. 12 AFMS: Scam targets mineral clubs ............ p. 13 Safety: Be prepared ................................... p. 13 Deadline for Submissions Field trip opportunity ................................. p. 14 November 20 Manassas quarry geology, pt. 2 ................. p. 15 Please make your submission by the 20th of the month! Upcoming events ....................................... p. 20 Submissions received later might go into a later newsletter. 28th Annual Show flyer ............................. p. 21 Mineral of the Month Datolite by Sue Marcus Datolite, our mineral this month, is not a zeolite, alt- hough it often occurs with minerals of the Zeolite Group. It can form lustrous crystals or attractive masses that take a nice polish. And, for collectors like Northern Virginia Mineral Club me, it is attainable! members, Etymology Please join our guest speaker, Joe Marx, for dinner at Datolite was named in 1806 by Jens Esmark, a Danish- the Olive Garden on November 18 at 6 p.m.
    [Show full text]
  • Report on the Sonora Lithium Project
    Report on the Sonora Lithium Project (Pursuant to National Instrument 43-101 of the Canadian Securities Administrators) Huasabas - Bacadehuachi Area (Map Sheet H1209) Sonora, Mexico o o centered at: 29 46’29”N, 109 6’14”W For 330 – 808 – 4th Avenue S. W. Calgary, Alberta Canada T2P 3E8 Tel. +1-403-237-6122 By Carl G. Verley, P. Geo. Martin F. Vidal, Lic. Geo. Geological Consultant Vice-President, Exploration Amerlin Exploration Services Ltd. Bacanora Minerals Ltd. 2150 – 1851 Savage Road Calle Uno # 312 Richmond, B.C. Canada V6V 1R1 Hermosillo, Mexico Tel. +1-604-821-1088 Tel. +52-662-210-0767 Ellen MacNeill, P.Geo. Geological Consultant RR5, Site25, C16 Prince Albert, SK Canada S6V 5R3 Tel. +1-306-922-6886 Dated: September 5, 2012. Bacanora Minerals Ltd. Report on the Sonora Lithium Project, Sonora, Mexico Date and Signature Page Date Dated Effective: September 5, 2012. Signatures Carl G. Verley, P.Geo. ____________________ Martin F. Vidal, Lic. Geo. Ellen MacNeill, P.Geo. Amerlin Exploration Services Ltd. - Consulting mineral exploration geologists ii Bacanora Minerals Ltd. Report on the Sonora Lithium Project, Sonora, Mexico Table of Contents 1.0 Summary ................................................................................................................................... 1 2.0 Introduction ............................................................................................................................... 3 3.0 Reliance on Other Experts .......................................................................................................
    [Show full text]