Asbestos Fibers and Other Elongate Mineral Particles: State of the Science and Roadmap for Research
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I`mt`qx1/00Lhmdq`knesgdLnmsg9Rbnkdbhsd This month’s mineral, scolecite, is an uncommon zeolite from India. Our write-up explains its origin as a secondary mineral in volcanic host rocks, the difficulty of collecting this fragile mineral, the unusual properties of the zeolite-group minerals, and why mineralogists recently revised the system of zeolite classification and nomenclature. OVERVIEW PHYSICAL PROPERTIES Chemistry: Ca(Al2Si3O10)A3H2O Hydrous Calcium Aluminum Silicate (Hydrous Calcium Aluminosilicate), usually containing some potassium and sodium. Class: Silicates Subclass: Tectosilicates Group: Zeolites Crystal System: Monoclinic Crystal Habits: Usually as radiating sprays or clusters of thin, acicular crystals or Hairlike fibers; crystals are often flattened with tetragonal cross sections, lengthwise striations, and slanted terminations; also massive and fibrous. Twinning common. Color: Usually colorless, white, gray; rarely brown, pink, or yellow. Luster: Vitreous to silky Transparency: Transparent to translucent Streak: White Cleavage: Perfect in one direction Fracture: Uneven, brittle Hardness: 5.0-5.5 Specific Gravity: 2.16-2.40 (average 2.25) Figure 1. Scolecite. Luminescence: Often fluoresces yellow or brown in ultraviolet light. Refractive Index: 1.507-1.521 Distinctive Features and Tests: Best field-identification marks are acicular crystal habit; vitreous-to-silky luster; very low density; and association with other zeolite-group minerals, especially the closely- related minerals natrolite [Na2(Al2Si3O10)A2H2O] and mesolite [Na2Ca2(Al6Si9O30)A8H2O]. Laboratory tests are often needed to distinguish scolecite from other zeolite minerals. Dana Classification Number: 77.1.5.5 NAME The name “scolecite,” pronounced SKO-leh-site, is derived from the German Skolezit, which comes from the Greek sklx, meaning “worm,” an allusion to the tendency of its acicular crystals to curl when heated and dehydrated. -
Articles Devoted to Silicate Minerals from Fumaroles of the Tol- Bachik Volcano (Kamchatka, Russia)
Eur. J. Mineral., 32, 101–119, 2020 https://doi.org/10.5194/ejm-32-101-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Unusual silicate mineralization in fumarolic sublimates of the Tolbachik volcano, Kamchatka, Russia – Part 1: Neso-, cyclo-, ino- and phyllosilicates Nadezhda V. Shchipalkina1, Igor V. Pekov1, Natalia N. Koshlyakova1, Sergey N. Britvin2,3, Natalia V. Zubkova1, Dmitry A. Varlamov4, and Eugeny G. Sidorov5 1Faculty of Geology, Moscow State University, Vorobievy Gory, 119991 Moscow, Russia 2Department of Crystallography, St Petersburg State University, University Embankment 7/9, 199034 St. Petersburg, Russia 3Kola Science Center of Russian Academy of Sciences, Fersman Str. 14, 184200 Apatity, Russia 4Institute of Experimental Mineralogy, Russian Academy of Sciences, Academica Osypyana ul., 4, 142432 Chernogolovka, Russia 5Institute of Volcanology and Seismology, Far Eastern Branch of Russian Academy of Sciences, Piip Boulevard 9, 683006 Petropavlovsk-Kamchatsky, Russia Correspondence: Nadezhda V. Shchipalkina ([email protected]) Received: 19 June 2019 – Accepted: 1 November 2019 – Published: 29 January 2020 Abstract. This is the initial paper in a pair of articles devoted to silicate minerals from fumaroles of the Tol- bachik volcano (Kamchatka, Russia). These papers contain the first systematic data on silicate mineralization of fumarolic genesis. In this article nesosilicates (forsterite, andradite and titanite), cyclosilicate (a Cu,Zn- rich analogue of roedderite), inosilicates (enstatite, clinoenstatite, diopside, aegirine, aegirine-augite, esseneite, “Cu,Mg-pyroxene”, wollastonite, potassic-fluoro-magnesio-arfvedsonite, potassic-fluoro-richterite and litidion- ite) and phyllosilicates (fluorophlogopite, yanzhuminite, “fluoreastonite” and the Sn analogue of dalyite) are characterized with a focus on chemistry, crystal-chemical features and occurrence. -
MINERALOGY for PETROLOGISTS Comprising a Guidebook and a Full Color CD-ROM, This Reference Set Offers Illustrated Essentials to Study Mineralogy, Applied to Petrology
MINERALOGY for PETROLOGISTS for MINERALOGY Comprising a guidebook and a full color CD-ROM, this reference set offers illustrated essentials to study mineralogy, applied to petrology. While there are some excellent reference works available on this subject, this work is unique for its data richness and its visual character. MINERALOGY for PETROLOGISTS With a collection of images that excels both in detail and aesthetics, 151 minerals are presented in more than 400 plates. Different facies and paragenesis, both in natural polarized light, are shown for every mineral and optical data, sketches of the crystal habitus, chemical composition, occurrence and a brief description are Optics, Chemistry and Occurrences included. The accompanying user guide gives a general introduction to microscope mineral observation, systematic mineralogy, mineral chemistry, occurrence, of Rock-Forming Minerals stability, paragenesis, structural formula calculation and its use in petrology. This compact set will serve as a field manual to students, researchers and Michel Demange professionals in geology, geological, mining, and mineral resources engineering to observe and determine minerals in their studies or field work. Dr. Michel Demange has devoted his career to regional geology and tectonics of metamorphic and magmatic terranes and to ore deposits. Graduated from the École Nationale Supérieure des Mines de Paris and holding a Docteur-es-Sciences from the University Pierre et Marie Curie, Paris VI, he has been active in a rich variety of geological projects and investigations around the world. In combination with his teaching and research activities at the École des Mines in Paris, France, he headed various research studies. This book benefits from the great experience in field M. -
A Comparative Study of Jadeite, Omphacite and Kosmochlor Jades from Myanmar, and Suggestions for a Practical Nomenclature
Feature Article A Comparative Study of Jadeite, Omphacite and Kosmochlor Jades from Myanmar, and Suggestions for a Practical Nomenclature Leander Franz, Tay Thye Sun, Henry A. Hänni, Christian de Capitani, Theerapongs Thanasuthipitak and Wilawan Atichat Jadeitite boulders from north-central Myanmar show a wide variability in texture and mineral content. This study gives an overview of the petrography of these rocks, and classiies them into ive different types: (1) jadeitites with kosmochlor and clinoamphibole, (2) jadeitites with clinoamphibole, (3) albite-bearing jadeitites, (4) almost pure jadeitites and (5) omphacitites. Their textures indicate that some of the assemblages formed syn-tectonically while those samples with decussate textures show no indication of a tectonic overprint. Backscattered electron images and electron microprobe analyses highlight the variable mineral chemistry of the samples. Their extensive chemical and textural inhomogeneity renders a classiication by common gemmological methods rather dificult. Although a deinitive classiication of such rocks is only possible using thin-section analysis, we demonstrate that a fast and non-destructive identiication as jadeite jade, kosmochlor jade or omphacite jade is possible using Raman and infrared spectroscopy, which gave results that were in accord with the microprobe analyses. Furthermore, current classiication schemes for jadeitites are reviewed. The Journal of Gemmology, 34(3), 2014, pp. 210–229, http://dx.doi.org/10.15506/JoG.2014.34.3.210 © 2014 The Gemmological Association of Great Britain Introduction simple. Jadeite jade is usually a green massive The word jade is derived from the Spanish phrase rock consisting of jadeite (NaAlSi2O6; see Ou Yang, for piedra de ijada (Foshag, 1957) or ‘loin stone’ 1999; Ou Yang and Li, 1999; Ou Yang and Qi, from its reputed use in curing ailments of the loins 2001). -
BURMESE JADE: the INSCRUTABLE GEM by Richard W
BURMESE JADE: THE INSCRUTABLE GEM By Richard W. Hughes, Olivier Galibert, George Bosshart, Fred Ward, Thet Oo, Mark Smith, Tay Thye Sun, and George E. Harlow The jadeite mines of Upper Burma (now Myanmar) occupy a privileged place in the If jade is discarded and pearls destroyed, petty thieves world of gems, as they are the principal source of top-grade material. This article, by the first will disappear, there being no valuables left to steal. foreign gemologists allowed into these impor- — From a dictionary published during the reign of tant mines in over 30 years, discusses the his- Emperor K’ang Hsi (1662–1722 AD) , as quoted by Gump, 1962 tory, location, and geology of the Myanmar jadeite deposits, and especially current mining erhaps no other gemstone has the same aura of mys- activities in the Hpakan region. Also detailed tery as Burmese jadeite. The mines’ remote jungle are the cutting, grading, and trading of location, which has been off-limits to foreigners for jadeite—in both Myanmar and China—as P well as treatments. The intent is to remove decades, is certainly a factor. Because of the monsoon rains, some of the mystery surrounding the Orient’s this area is essentially cut off from the rest of the world for most valued gem. several months of the year, and guerrilla activities have plagued the region since 1949 (Lintner, 1994). But of equal importance is that jade connoisseurship is almost strictly a Chinese phenomenon. People of the Orient have developed jade appreciation to a degree found nowhere else in the world, but this knowledge is largely locked away ABOUT THE AUTHORS in non-Roman-alphabet texts that are inaccessible to most Mr. -
Anto A, Larson C, Horton D. 2012. Libby Vermiculite Exposure And
REVIEW CURRENT OPINION Libby vermiculite exposure and risk of developing asbestos-related lung and pleural diseases Vinicius C. Antao, Theodore C. Larson, and D. Kevin Horton Purpose of review The vermiculite ore formerly mined in Libby, Montana, contains asbestiform amphibole fibers of winchite, richterite, and tremolite asbestos. Because of the public health impact of widespread occupational and nonoccupational exposure to amphiboles in Libby vermiculite, numerous related studies have been published in recent years. Here we review current research related to this issue. Recent findings Excess morbidity and mortality classically associated with asbestos exposure have been well documented among persons exposed to Libby vermiculite. Excess morbidity and mortality have likewise been documented among persons with only nonoccupational exposure. A strong exposure–response relationship exists for many malignant and nonmalignant outcomes and the most common outcome, pleural plaques, may occur at low lifetime cumulative exposures. Summary The public health situation related to Libby, Montana, has led to huge investments in public health actions and research. The resulting studies have added much to the body of knowledge concerning health effects of exposures to Libby amphibole fibers specifically and asbestos exposure in general. Keywords amphibole, asbestos, Libby, respiratory diseases, vermiculite INTRODUCTION Libby vermiculite was shipped throughout the US to A vermiculite mine and mill located near Libby, more than 200 domestic processing and receiving Montana, operated from the early 1920s until facilities [6]. Interestingly, the first identification by 1990. Vermiculite is a naturally occurring laminar public health authorities of pulmonary abnormal- aluminum-iron-magnesium silicate. It expands ities associated with Libby vermiculite concerned when heated, and has been employed in many exposures outside of Libby. -
Description and Recognition of Potassic-Richterite, an Amphibole Supergroup Mineral from the Pajsberg Ore Field, Värmland, Sweden
Mineralogy and Petrology (2019) 113:7–16 https://doi.org/10.1007/s00710-018-0623-6 ORIGINAL PAPER Description and recognition of potassic-richterite, an amphibole supergroup mineral from the Pajsberg ore field, Värmland, Sweden Dan Holtstam1 & Fernando Cámara2 & Henrik Skogby1 & Andreas Karlsson1 & Jörgen Langhof1 Received: 17 April 2018 /Accepted: 12 July 2018 /Published online: 10 August 2018 # The Author(s) 2018 Abstract A B C T W Potassic-richterite, ideally K (NaCa) Mg5 Si8O22 (OH)2, is recognized as a valid member of the amphibole supergroup (IMA- CNMNC 2017–102). Type material is from the Pajsberg Mn-Fe ore field, Filipstad, Värmland, Sweden, where the mineral occurs in a Mn-rich skarn, closely associated with mainly phlogopite, jacobsite and tephroite. The megascopic colour is straw yellow to grayish brown and the luster vitreous. The nearly anhedral crystals, up to 4 mm in length, are pale yellow (non-pleochroic) in thin section and −1 optically biaxial (−), with α = 1.615(5), β = 1.625(5), γ = 1.635(5). The calculated density is 3.07 g·cm . VHN100 is in the range 610– 946. Cleavage is perfect along {110}. EPMA analysis in combination with Mössbauer and infrared spectroscopy yields the empirical 3+ 3+ formula (K0.61Na0.30Pb0.02)∑0.93(Na1.14Ca0.79Mn0.07)∑2(Mg4.31Mn0.47Fe 0.20)∑5(Si7.95Al0.04Fe 0.01)∑8O22(OH1.82F0.18)∑2 for a frag- ment used for collection of single-crystal X-ray diffraction data. The infra-red spectra show absorption bands at 3672 cm−1 and 3736 cm−1 for the α direction. -
Newsletter of the New York Microscopical Society
Newsletter Of the New York Microscopical Society 1 Prospect Village Plaza (66F Mt. Prospect Avenue) Clifton, New Jersey 07013-1918 GPS: Latitude 40.8648N, Longitude 74.1540W Nov-Dec 2016 Editor: (201) 791-9826 Volume 10 (30) Number 9 NYMS ANNUAL BANQUET DECEMBER 11, 2016 What: Enjoy a wonderful Buffet Luncheon, including soft beverages (cash bar available) and desserts, with your fellow-members and guests. Enjoy an exciting presentation by Asst. Professor Nicholas Petraco, MS, D-ABC John Jay College of Criminal Justice (See page 3 for add’l info). An overall jolly time at one of the oldest restaurants in mid-town Manhattan; The Landmark Tavern. When: Sunday December 11, 2016, from noon until 3:30pm. Where: Landmark Tavern, 626 11th Ave., at W. 46th St New York City, NY Tel: 212-247-2562. Cost: $35.00 per person. How: Reserve your place now* by filling in the Reservation Request form below and mailing it along with your check to the Treasurer (see address below). *Reservation requests must be received on or before November 28, 2016 ------------------------------------------------------------------------------------------------------------------------ Number attending _________ @ $35/each = (write check amount) _______ Member name______________________________________________ Address____________________________________________________ Phone__________________ eMail____________________ ________________________________________________________________ Send this form and payment to: NYMS Banquet 2016 c/o Mel Pollinger, Treasurer 18-04 Hillery Street Fair Lawn, NJ 07410-5207 For additional information contact Mel Pollinger (201) 791-9826 or email: [email protected] Space is limited, so rush your reservation request in to reserve your place(s) asap. A Not-For-Profit Educational Organization, (nyms.org) Save a Tree: Get The Extended Newsletter: By Email Only New York Microscopical Society Board of Managers (Officers Term 2016-2017) President, John Scott, [email protected]; (646)339-6566, Curator, Archivist. -
Characterization of Fibrous Mordenite: a First Step for the Evaluation of Its Potential Toxicity
crystals Article Characterization of Fibrous Mordenite: A First Step for the Evaluation of Its Potential Toxicity Dario Di Giuseppe 1,2 1 Department of Chemical and Geological Sciences, University of Modena and Reggio Emilia, Via G. Campi 103, I-41125 Modena, Italy; [email protected] 2 Department of Sciences and Methods for Engineering, University of Modena and Reggio Emilia, Via Amendola 2, I-42122 Reggio Emilia, Italy Received: 4 August 2020; Accepted: 28 August 2020; Published: 31 August 2020 Abstract: In nature, a huge number of unregulated minerals fibers share the same characteristics as asbestos and therefore have potential adverse health effects. However, in addition to asbestos minerals, only fluoro-edenite and erionite are currently classified as toxic/pathogenic agents by the International Agency for Research on Cancer (IARC). Mordenite is one of the most abundant zeolites in nature and commonly occurs with a fibrous crystalline habit. The goal of this paper is to highlight how fibrous mordenite shares several common features with the well-known carcinogenic fibrous erionite. In particular, this study has shown that the morphology, biodurability, and surface characteristics of mordenite fibers are similar to those of erionite and asbestos. These properties make fibrous mordenite potentially toxic and exposure to its fibers can be associated with deadly diseases such as those associated with regulated mineral fibers. Since the presence of fibrous mordenite concerns widespread geological formations, this mineral fiber should be considered dangerous for health and the precautionary approach should be applied when this material is handled. Future in vitro and in vivo tests are necessary to provide further experimental confirmation of the outcome of this work. -
Meeker Et Al. 2003. the Composition of Amphiboles from the Rainy
American Mineralogist, Volume 88, pages 1955–1969, 2003 The Composition and Morphology of Amphiboles from the Rainy Creek Complex, Near Libby, Montana G.P. MEEKER,1,* A.M. BERN,1 I.K. BROWNFIELD,1 H.A. LOWERS,1,2 S.J. SUTLEY,1 T.M. HOEFEN,1 AND J.S.VANCE3 1U.S. Geological Survey, Denver Microbeam Laboratory, Denver, Colorado 80225, U.S.A. 2Colorado School of Mines, Golden, Colorado, 80401, U.S.A. 3U.S. Environmental Protection Agency, Region 8, Denver, Colorado 80204, U.S.A. ABSTRACT Thirty samples of amphibole-rich rock from the largest mined vermiculite deposit in the world in the Rainy Creek alkaline-ultramafic complex near Libby, Montana, were collected and analyzed. The amphibole-rich rock is the suspected cause of an abnormally high number of asbestos-related diseases reported in the residents of Libby, and in former mine and mill workers. The amphibole-rich samples were analyzed to determine composition and morphology of both fibrous and non-fibrous amphiboles. Sampling was carried out across the accessible portions of the deposit to obtain as complete a representation of the distribution of amphibole types as possible. The range of amphibole compositions, determined from electron probe microanalysis and X-ray diffraction analysis, indi- cates the presence of winchite, richterite, tremolite, and magnesioriebeckite. The amphiboles from Vermiculite Mountain show nearly complete solid solution between these end-member composi- tions. Magnesio-arfvedsonite and edenite may also be present in low abundance. An evaluation of the textural characteristics of the amphiboles shows the material to include a complete range of morphologies from prismatic crystals to asbestiform fibers. -
TVA Best Practices Procedural Guide
Asbestos Detection and Control Protocol: Vermiculite Mining and Milling PROCEDURAL GUIDE Contents Introduction: Asbestos and Mineral Fibres ................................................................... 2 Asbestos Mineral .............................................................................................................. 2 Definition of Asbestos .................................................................................................. 3 Quality Control Systems ............................................................................................... 5 Management and Technical Training ............................................................................ 6 Asbestos Control Procedures ....................................................................................... 7 Mine Ore Body – Pre‐Extraction ....................................................................................... 7 Processed Vermiculite ...................................................................................................... 8 External Laboratory Testing of Vermiculite Product Samples .......................................... 9 Safe Management, Disposal and Handling ...................................................................... 9 Analytical Test Procedures ......................................................................................... 10 Laboratory Equipment (TVA Recommended Method) ................................................... 10 Stereomicroscopy .......................................................................................................... -
Natural Zeolites Filling Amygdales and Veins in Basalts from the British Tertiary Igneous Province on the Isle of Skye, Scotland
EARTH SCIENCES RESEARCH JOURNAL Earth Sci Res SJ Vol 16, No 1 (June, 2012): 41 - 53 PETROLOGY Natural zeolites filling amygdales and veins in basalts from the British Tertiary Igneous Province on the Isle of Skye, Scotland Juan Manuel Triana R 1, Javier Francisco Herrera R 1, Carlos Alberto Ríos R 1*, Oscar Mauricio Castellanos A 2, José Antonio Henao M 3, Craig D Williams4 and Clive L Roberts4 1* Escuela de Geología, Universidad Industrial de Santander, Bucaramanga, Colombia 2 Programa de Geología, Universidad de Pamplona, Colombia 3 Grupo de Investigación en Química Estructural (GIQUE), Escuela de Química - Universidad Industrial de Santander 4 School of Applied Sciences, University of Wolverhampton, England * Corresponding author E-mail: carios@uis edu co Abstract Keywords: natural zeolite, amygdale, vein, basaltic rock, Isle of Skye Natural zeolites filling amygdales and veins in tertiary basaltic host rocks on the Isle of Skye (NW Scotland) have been studied in some detail by transmitted light microscopy, scanning electron microscopy and X-ray diffraction techniques The zeolites and associated minerals so identified in order of their relative time of for- mation from early to late were nontronite, amorphous silica phases, carbonate phases, chabazite, phillipsite, wairakite, thomsonite, analcime, natrolite and stilbite-type minerals Zeolite formation in the Skye basalts began with low Si/Al ratio Na zeolites and a gradual increase in Ca content and Si/Al ratio, ending up as Ca zeolites They were probably formed as a consequence of