Thirty-Third List of New Mineral Names
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Genesis of Chah-Talkh Nonsulfide Zn-Pb Deposit (South of Iran): Evidence from Geology, Mineralogy, Geochemistry and Stable Isotope (C, O) Data --Manuscript Draft
Arabian Journal of Geosciences Genesis of Chah-Talkh nonsulfide Zn-Pb deposit (south of Iran): Evidence from Geology, Mineralogy, Geochemistry and Stable Isotope (C, O) data --Manuscript Draft-- Manuscript Number: AJGS-D-12-00257 Full Title: Genesis of Chah-Talkh nonsulfide Zn-Pb deposit (south of Iran): Evidence from Geology, Mineralogy, Geochemistry and Stable Isotope (C, O) data Article Type: Original Paper Abstract: Abstract Chah-Talkh nonsulfide Zn-Pb deposit with about more than 720000 t at 15% Zn in the form of Zn carbonates and silicates is a target resource in the south of Iran. In this preliminary study, some cases likes geology, mineralogy and geochemistry (major and trace element data and stable Isotope) of this deposit in surface and depth are investigated for determine of genesis. The analyses carried out on samples from 14 drill cores and 15 surface profiles (vertical to veins strike). Mineralization occurs in 3 main veins with thickness about 0.5 to 3 meters in the length about 900 m that in (resent) exploration this length increases. Main ore minerals are hydrozincite, hemimorphite and smithsonite. The mineralogical and geochemical evidences indicate that Chah-Talkh deposit is a typical supergene nonsulfide Zn-Pb deposit in carbonate rocks that primary sulfide ores almost has been affected by deeply weathered. Mineralization in Chah-Talkh is generally associated with fracture zones and dolomitization. It seems that distribution of hemimorphite, smithsonite and hydrozincite is reflection of existing of clay minerals in host rocks. In presence of clay minerals (in marly limestone) main ore mineral is hemimorphite and in absence of clay minerals (micritic limestone) main ore mineral is hydrozincite and smithsonite. -
Iseite, Mn2mo3o8, a New Mineral from Ise, Mie Prefecture, Japan
Journal of Mineralogical and PetrologicalIseite, a new Sciences, mineral Volume 108, page 37─ 41, 2013 37 LETTER Iseite, Mn2Mo3O8, a new mineral from Ise, Mie Prefecture, Japan * ** ** *** Daisuke NISHIO-HAMANE , Norimitsu TOMITA , Tetsuo MINAKAWA and Sachio INABA * The institute for Solid State Physics, University of Tokyo, Kashiwa, Chiba 277-8581, Japan ** Department of Earth Science, Faculty of Science, Ehime University, Matsuyama, Ehime 790-8577, Japan *** Inaba-Shinju Corporation, Minamiise, Mie 516-0109, Japan Iseite, Mn2Mo3O8, a new mineral that is a Mn-dominant analogue of kamiokite, is found in the stratiform ferro- manganese deposit, Shobu area, Ise City, Mie Prefecture, Japan. It is the first mineral species that includes both Mn and Mo as essential constituents. Iseite is iron-black in color and has a submetallic luster. It occurs as ag- gregates up to about 1 mm in size made of minute crystals (<20 μm). Iseite has a zoned structure closely associ- ated with undetermined Mn-Fe-Mo oxide minerals with hexagonal forms, and it occasionally coexists with 3 small amounts of powellite. Its Mohs hardness is 4-5, and its calculated density is 5.85 g/cm . The empirical formula of iseite is (Mn1.787Fe0.193)Σ1.980Mo3.010O8. Its simplified ideal formula is written as Mn2Mo3O8. The min- eral is isostructural with kamiokite (hexagonal, P63mc). The unit cell parameters are a = 5.8052 (3) Å, c = 10.2277 (8) Å, V = 298.50 (4) Å3, and Z = 2. The Rietveld refinement using synchrotron radiation (λ = 0.413 Å) powder XRD data converges to Rwp = 3.11%, and confirms two independent Mn sites—tetrahedral and octahe- IV VI dral—in the crystal structure of iseite, indicating the structure formula Mn Mn Mo3O8. -
George Robert Rossman Feb 15, 1995
George Robert Rossman 20-Jun-2020 Present Position: Professor of Mineralogy Option Representative for Geochemistry Division of Geological and Planetary Sciences California Institute of Technology Pasadena, California 91125-2500 Office Telephone: (626)-395-6471 FAX: (626)-568-0935 E-mail: [email protected] Residence: Pasadena, California Birthdate: August 3, l944, LaCrosse, Wisconsin Education: B.S. (Chemistry and Mathematics), Wisconsin State University, Eau Claire, 1966, Summa cum Laude Ph.D. (Chemistry), California Institute of Technology, Pasadena, 1971 Experience: California Institute of Technology Division of Geological and Planetary Sciences a) 1971 Instructor in Mineralogy b) 1971-1974 Assistant Professor of Mineralogy and Chemistry c) 1974-1977 Assistant Professor of Mineralogy d) 1977-1984 Associate Professor of Mineralogy e) 1984-2008 Professor of Mineralogy f) 2008-2015 Eleanor and John R. McMillan Professor of Mineralogy e) 2015- Professor of Mineralogy Principal Research Interests: a) Spectroscopic studies of minerals. These studies include problems relating to the origin of color phenomena in minerals; site ordering in crystals; pleochroism; metal ions in distorted sites; analytical applications. b) The role of low concentrations of water and hydroxide in nominally anhydrous solids. Analytical methods for OH analysis, mode of incorporation, role of OH in modifying physical and chemical properties, and its relationship to conditions of formation in the natural environment. c) Long term radiation damage effects in minerals from background levels of natural radiation. The effects of high level ionizing radiation on minerals. d) X-ray amorphous minerals. These studies have involved the physical chemical study of bioinorganic hard parts of marine organisms and products of terrestrial surface weathering, and metamict minerals. -
Washington State Minerals Checklist
Division of Geology and Earth Resources MS 47007; Olympia, WA 98504-7007 Washington State 360-902-1450; 360-902-1785 fax E-mail: [email protected] Website: http://www.dnr.wa.gov/geology Minerals Checklist Note: Mineral names in parentheses are the preferred species names. Compiled by Raymond Lasmanis o Acanthite o Arsenopalladinite o Bustamite o Clinohumite o Enstatite o Harmotome o Actinolite o Arsenopyrite o Bytownite o Clinoptilolite o Epidesmine (Stilbite) o Hastingsite o Adularia o Arsenosulvanite (Plagioclase) o Clinozoisite o Epidote o Hausmannite (Orthoclase) o Arsenpolybasite o Cairngorm (Quartz) o Cobaltite o Epistilbite o Hedenbergite o Aegirine o Astrophyllite o Calamine o Cochromite o Epsomite o Hedleyite o Aenigmatite o Atacamite (Hemimorphite) o Coffinite o Erionite o Hematite o Aeschynite o Atokite o Calaverite o Columbite o Erythrite o Hemimorphite o Agardite-Y o Augite o Calciohilairite (Ferrocolumbite) o Euchroite o Hercynite o Agate (Quartz) o Aurostibite o Calcite, see also o Conichalcite o Euxenite o Hessite o Aguilarite o Austinite Manganocalcite o Connellite o Euxenite-Y o Heulandite o Aktashite o Onyx o Copiapite o o Autunite o Fairchildite Hexahydrite o Alabandite o Caledonite o Copper o o Awaruite o Famatinite Hibschite o Albite o Cancrinite o Copper-zinc o o Axinite group o Fayalite Hillebrandite o Algodonite o Carnelian (Quartz) o Coquandite o o Azurite o Feldspar group Hisingerite o Allanite o Cassiterite o Cordierite o o Barite o Ferberite Hongshiite o Allanite-Ce o Catapleiite o Corrensite o o Bastnäsite -
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 -
Uraninite Alteration in an Oxidizing Environment and Its Relevance to the Disposal of Spent Nuclear Fuel
TECHNICAL REPORT 91-15 Uraninite alteration in an oxidizing environment and its relevance to the disposal of spent nuclear fuel Robert Finch, Rodney Ewing Department of Geology, University of New Mexico December 1990 SVENSK KÄRNBRÄNSLEHANTERING AB SWEDISH NUCLEAR FUEL AND WASTE MANAGEMENT CO BOX 5864 S-102 48 STOCKHOLM TEL 08-665 28 00 TELEX 13108 SKB S TELEFAX 08-661 57 19 original contains color illustrations URANINITE ALTERATION IN AN OXIDIZING ENVIRONMENT AND ITS RELEVANCE TO THE DISPOSAL OF SPENT NUCLEAR FUEL Robert Finch, Rodney Ewing Department of Geology, University of New Mexico December 1990 This report concerns a study which was conducted for SKB. The conclusions and viewpoints presented in the report are those of the author (s) and do not necessarily coincide with those of the client. Information on SKB technical reports from 1977-1978 (TR 121), 1979 (TR 79-28), 1980 (TR 80-26), 1981 (TR 81-17), 1982 (TR 82-28), 1983 (TR 83-77), 1984 (TR 85-01), 1985 (TR 85-20), 1986 (TR 86-31), 1987 (TR 87-33), 1988 (TR 88-32) and 1989 (TR 89-40) is available through SKB. URANINITE ALTERATION IN AN OXIDIZING ENVIRONMENT AND ITS RELEVANCE TO THE DISPOSAL OF SPENT NUCLEAR FUEL Robert Finch Rodney Ewing Department of Geology University of New Mexico Submitted to Svensk Kämbränslehantering AB (SKB) December 21,1990 ABSTRACT Uraninite is a natural analogue for spent nuclear fuel because of similarities in structure (both are fluorite structure types) and chemistry (both are nominally UOJ. Effective assessment of the long-term behavior of spent fuel in a geologic repository requires a knowledge of the corrosion products produced in that environment. -
Weeksite K2(UO2)2(Si5o13)·4H2O
Weeksite K2(UO2)2(Si5O13)·4H2O Crystal Data: Monoclinic. Point Group: 2/m: As bladed or acicular crystals, flattened on {010} and elongated along [001], and as flat plates; also as spherulites and radiating fibrous clusters. - Twinning: By two-fold rotation around [401 ]. Physical Properties: Cleavage: Two good prismatic cleavages noted. Hardness = < 2 D(meas.) = ~ 4.1 D(calc.) = 3.80 Radioactive. Optical Properties: Transparent to translucent. Color: Yellow. Luster: Waxy to silky. Optical Class: Biaxial (-). α = 1.596 β = 1.603 γ = 1.606 2V(meas.) = ~ 60° 2V(calc.) = 66° Pleochroism: X = colorless, Y = pale yellow-green, Z = yellow-green. Dispersion: r > v, strong. Orientation: X = b, Y = c, Z = a. Cell Data: Space Group: C2/m. a = 14.26(2) b = 35.88(10) c = 14.20(2) β = 111.578(3)° Z = 4 X-ray Powder Pattern: Thomas Range, Utah, USA. 7.11 (10), 5.57 (9), 8.98 (8), 3.55 (7), 3.30 (7), 2.91 (6), 3.20 (5) Chemistry: (1) (1) Na2O 0.53 Al2O3 0.6 K2O 4.73 SiO2 29.44 CaO 0.67 UO3 55.78 BaO 3.11 H2O [7.02] MgO 0.18 Total 101.28 SrO 0.20 (1) Anderson mine, Arizona, USA; average of 8 electron microprobe analyses, supplemented by TGA, H2O calculated from structure, corresponds to (K1.031Na0.176Ca0.123Ba0.208)Σ=1.537(UO2)2.002 (Si5.030O13)·4H2O. Occurrence: In “opal" veinlets in rhyolite, agglomerates, sandstones and limestones. Association: “Opal," “chalcedony," calcite, gypsum, fluorite, uraninite, thorogummite, uranophane, boltwoodite, carnotite, margaritasite. Distribution: In the USA, in Utah, at the Autunite No. -
Jarosewichite and a Related Phase: Basic Manganese Arsenates of the Chlorophoenicite Group from Franklin, New Jersey
American Mineralogist, Volume 67, pages 1043-1047,1962 Jarosewichite and a related phase: basic manganese arsenates of the chlorophoenicite group from Franklin, New Jersey Pe,re J. DUNN Department of Mineral Sciences Smit hsonian I nstit utio n Washington, D.C.20560 DoNelo R. Pr,econ Department of Geological Sciences University of Michigan Ann Arbor, Michigan 48109 PBrBn B. LBeveNs Department of Geology University of Delaware Newark, Delaware l97II eNo Wrllreu B. SIuuoNs Department of Earth Sciences University of New Orleans New Orleans. Louisiana 70148 Abstract Jarosewichite,Mn3+Mn3+(AsOn)(OH)0, is a new mineral, closely related to chloro- phoenicite,from the Franklin mine, Franklin, SussexCounty, New Jersey,where it occurs associatedwith andradite,franklinite, flinkite, cahniteand hausmannite.Jarosewichite is orthorhombic,space grotp C2lmLlm2lm,C222 or Cmm2,with a : 6.56(3),b : 25.20(10),c : 10.00(5)4,and Z : 8. The strongestlines in the X-ray powder difraction patternare (d, I, hkD2.669 100 222,082;3.91 60 042,061;1.788 50 (notindexed);2.503 30 242,261,004,0 l0 0. Jarosewichiteis dark red, occursin prismaticbarrel-shaped aggregates, has a density of 3.66(obs),3.70glcm3(calc).Itisbiaxial(-)withrefractiveindicesd= 1.780(5),p= 1.795(5)and y= 1.805(5);theorientationisX:a,Y: b,Z = c;pleochroismisweak,Z) X. Microprobeanalysis with Mn3+calculated, yields: FeO 0.4, MgO 2.l,CaO0.2,ZnO 1.2, MnO 42.3, Mn2O317.7 (IMn = 45.1 wt.%), AszOs24.0, with H2O 12.1 percent by difference,sum : 100.0percent. A secondmanganese arsenate from Franklin, New Jersey,is alsorelated to chlorophoen- icite, but may be heterogeneous.Although optical, chemicaland crystallographicproper- ties are characterized,there is sufficient ambiguity to deny it speciesstatus at this time. -
Minerals Named After Scientists
Dr. John Andraos, http://www.careerchem.com/NAMED/Minerals.pdf 1 MINERALS NAMED AFTER PEOPLE AND PLACES © Dr. John Andraos, 2003-2011 Department of Chemistry, York University 4700 Keele Street, Toronto, ONTARIO M3J 1P3, CANADA For suggestions, corrections, additional information, and comments please send e-mails to [email protected] http://www.chem.yorku.ca/NAMED/ PEOPLE MINERAL PERSON OR PLACE DESCRIPTION Abelsonite ABELSON, Philip Hauge (1913 - ?) geochemist Abenakiite ABENAKI people, Quebec, Canada Abernathyite ABERNATHY, Jess Mine operator American, b. ? Abswurmbachite ABS-WURMBACH, IRMGARD (1938 - ) mineralogist German, b. ? Adamite ADAM, Gilbert Joseph Zn3(AsO3)2 H2O (1795 - 1881) mineralogist French, b. ? Aegirine AEGIR, Scandinavian god of the sea Afwillite WILLIAMS, Alpheus Fuller (1874 - ?) mine operator DeBeers Consolidated Mines, Kimberley, South Africa Agrellite AGRELL, Stuart O. (? - 1996) mineralogist British, b. ? Agrinierite AGRINIER, Henri (1928 - 1971) mineralogist French, b. ? Aguilarite AGUILAR, P. Superintendent of San Carlos mine, Guanajuato, Mexico Mexican, b. ? Aikenite 2 PbS Cu2S Bi2S5 Andersonite ANDERSON, Dr. John Andraos, http://www.careerchem.com/NAMED/Minerals.pdf 2 Andradite ANDRADA e Silva, Jose B. Ca3Fe2(SiO4)3 de (? - 1838) geologist Brazilian, b. ? Arfvedsonite ARFVEDSON, Johann August (1792 - 1841) Swedish, b. Skagerholms- Bruk, Skaraborgs-Län, Sweden Arrhenite ARRHENIUS, Svante Silico-tantalate of Y, Ce, Zr, (1859 - 1927) Al, Fe, Ca, Be Swedish, b. Wijk, near Uppsala, Sweden Avogardrite AVOGADRO, Lorenzo KBF4, CsBF4 Romano Amedeo Carlo (1776 - 1856) Italian, b. Turin, Italy Babingtonite (Ca, Fe, Mn)SiO3 Fe2(SiO3)3 Becquerelite BECQUEREL, Antoine 4 UO3 7 H2O Henri César (1852 - 1908) French b. Paris, France Berzelianite BERZELIUS, Jöns Jakob Cu2Se (1779 - 1848) Swedish, b. -
New Minerals Approved Bythe Ima Commission on New
NEW MINERALS APPROVED BY THE IMA COMMISSION ON NEW MINERALS AND MINERAL NAMES ALLABOGDANITE, (Fe,Ni)l Allabogdanite, a mineral dimorphous with barringerite, was discovered in the Onello iron meteorite (Ni-rich ataxite) found in 1997 in the alluvium of the Bol'shoy Dolguchan River, a tributary of the Onello River, Aldan River basin, South Yakutia (Republic of Sakha- Yakutia), Russia. The mineral occurs as light straw-yellow, with strong metallic luster, lamellar crystals up to 0.0 I x 0.1 x 0.4 rnrn, typically twinned, in plessite. Associated minerals are nickel phosphide, schreibersite, awaruite and graphite (Britvin e.a., 2002b). Name: in honour of Alia Nikolaevna BOG DAN OVA (1947-2004), Russian crys- tallographer, for her contribution to the study of new minerals; Geological Institute of Kola Science Center of Russian Academy of Sciences, Apatity. fMA No.: 2000-038. TS: PU 1/18632. ALLOCHALCOSELITE, Cu+Cu~+PbOZ(Se03)P5 Allochalcoselite was found in the fumarole products of the Second cinder cone, Northern Breakthrought of the Tolbachik Main Fracture Eruption (1975-1976), Tolbachik Volcano, Kamchatka, Russia. It occurs as transparent dark brown pris- matic crystals up to 0.1 mm long. Associated minerals are cotunnite, sofiite, ilin- skite, georgbokiite and burn site (Vergasova e.a., 2005). Name: for the chemical composition: presence of selenium and different oxidation states of copper, from the Greek aA.Ao~(different) and xaAxo~ (copper). fMA No.: 2004-025. TS: no reliable information. ALSAKHAROVITE-Zn, NaSrKZn(Ti,Nb)JSi401ZJz(0,OH)4·7HzO photo 1 Labuntsovite group Alsakharovite-Zn was discovered in the Pegmatite #45, Lepkhe-Nel'm MI. -
Optical Properties of Solar Cells Based on Zinc(Hydr)Oxide and Its Composite with Graphite Oxide Sensitized by Quantum Dots
City University of New York (CUNY) CUNY Academic Works All Dissertations, Theses, and Capstone Projects Dissertations, Theses, and Capstone Projects 2-2014 Optical Properties of Solar Cells Based on Zinc(hydr)oxide and its Composite with Graphite oxide Sensitized by Quantum Dots S. M. Zakirul Islam Graduate Center, City University of New York How does access to this work benefit ou?y Let us know! More information about this work at: https://academicworks.cuny.edu/gc_etds/54 Discover additional works at: https://academicworks.cuny.edu This work is made publicly available by the City University of New York (CUNY). Contact: [email protected] Optical Properties of Solar Cells Based on Zinc(hydr)oxide and its Composite with Graphite oxide Sensitized by Quantum Dots by S.M. Zakirul Islam A dissertation submitted to the Graduate Faculty in Electrical Engineering in partial fulfillment of the requirements for the degree of Doctor of Philosophy, The City University of New York 2014 © 2014 S.M. Zakirul Islam All Rights Reserved II This manuscript has been read and accepted for the Graduate Faculty of Electrical Engineering in satisfaction of the dissertation requirement for the degree of Doctor of Philosophy. Professor Robert R. Alfano Date Chair of Examining Committee Professor Ardie Walser Date Executive Officer Professor Joseph Birman Professor Ping Pei-Ho Professor Teresa J. Bandosz Professor Sang Woo Seo Dr. Wubao Wang Supervisory Committee The City University of New York III Abstract Optical Properties of Solar Cells Based on Zinc(hydr)oxide and its Composite with Graphite oxide Sensitized by Quantum Dots by S.M. -
Downloaded for Personal Non-Commercial Research Or Study, Without Prior Permission Or Charge
MacArtney, Adrienne (2018) Atmosphere crust coupling and carbon sequestration on early Mars. PhD thesis. http://theses.gla.ac.uk/9006/ Copyright and moral rights for this work are retained by the author A copy can be downloaded for personal non-commercial research or study, without prior permission or charge This work cannot be reproduced or quoted extensively from without first obtaining permission in writing from the author The content must not be changed in any way or sold commercially in any format or medium without the formal permission of the author When referring to this work, full bibliographic details including the author, title, awarding institution and date of the thesis must be given Enlighten:Theses http://theses.gla.ac.uk/ [email protected] ATMOSPHERE - CRUST COUPLING AND CARBON SEQUESTRATION ON EARLY MARS By Adrienne MacArtney B.Sc. (Honours) Geosciences, Open University, 2013. Submitted in partial fulfilment of the requirements for the degree of Doctor of Philosophy at the UNIVERSITY OF GLASGOW 2018 © Adrienne MacArtney All rights reserved. The author herby grants to the University of Glasgow permission to reproduce and redistribute publicly paper and electronic copies of this thesis document in whole or in any part in any medium now known or hereafter created. Signature of Author: 16th January 2018 Abstract Evidence exists for great volumes of water on early Mars. Liquid surface water requires a much denser atmosphere than modern Mars possesses, probably predominantly composed of CO2. Such significant volumes of CO2 and water in the presence of basalt should have produced vast concentrations of carbonate minerals, yet little carbonate has been discovered thus far.