United States Patent Office Patented May 30, 1967 1
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United States Patent (19) 11) 4,080,491 Kobayashi Et Al
United States Patent (19) 11) 4,080,491 Kobayashi et al. 45) Mar. 21, 1978 54) PROCESS OF PRODUCING RING-OPENING 56 References Cited POLYMERIZATION PRODUCTS U.S. PATENT DOCUMENTS (75) Inventors: Yukio Kobayashi; Takashi Ueshima; 3,798,175 3/1974 Streck .................................. 526/136 Shoichi Kobayashi, all of Yokohama, 3,856,758 - 12/1974 Ueshima ............................... 526/169 Japan 3,859,265 1/1975 Hepworth ............................ 526/281 3,959,234 5/1976 Kurosawa ............................ 526/281 Assignee: Showa Denko K.K., Tokyo, Japan (73) Primary Examiner-Paul R. Michl 21 Appl. No.: 714,833 Attorney, Agent, or Firm-Fitzpatrick, Cella, Harper & 22) Filed: Aug. 16, 1976 Scinto Foreign Application Priority Data 57 ABSTRACT (30) A process of producing a ring-opening polymerization Aug. 27, 1975 Japan ................................ 50-103060 product of a norbornene derivative containing at least Mar. 26, 1976 Japan .................................. 51-32464 one polar group or aromatic group, a norbornadiene Mar. 26, 1976 Japan .................................. 51-32465 derivative containing at least one of said groups or a Apr. 5, 1976 Japan .................................. 51-37274 cycloolefin using a catalyst system prepared from an Apr. 27, 1976 Japan .................................. 51-47268 organometallic compound and the reaction product of May 25, 1976 Japan .................................. 51-59642 tungsten oxide or molybdenum oxide and a phosphorus 51 Int. C.’................................................ C08F 4/78 pentahalide or phosphorus oxytrihalide or these com (52) U.S. C. ..... o e s p s 8 v 8 526/137; 526/113; pounds and other third components. The catalyst sys 526/127; 526/136; 526/169; 526/281; 526/308 temi possesses a high polymerization activity. (58) Field of Search .................... -
Cesstibtantite Cs(Sb3+
3+ Cesstibtantite Cs(Sb , Na)Ta2(O, OH, F)7 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Cubic. Point Group: 4/m 32/m. As cubo-octahedral crystals; granular, to 3 mm. Physical Properties: Fracture: Uneven. Tenacity: Brittle. Hardness = ∼5 VHN = 670– 780 (100 g load). D(meas.) = 6.4–6.6 D(calc.) = 6.49 Fluoresces yellow-orange to orange under LW UV; weak yellowish cathodoluminescence. Optical Properties: Transparent; may be opaque except in thinnest fragments. Color: Colorless to gray, yellow-orange, black. Luster: Adamantine to vitreous. Optical Class: Isotropic. n = > 1.8 R: (480) 13.8, (551) 13.6, (589) 13.6, (656) 13.0 Cell Data: Space Group: Fd3m. a = 10.496–10.515 Z = 8 X-ray Powder Pattern: Kola Peninsula, Russia. 3.04 (10), 1.860 (10), 1.587 (10), 1.012 (10), 3.17 (9), 1.370 (9), 1.017 (9) Chemistry: (1) (2) (3) (1) (2) (3) Nb2O5 2.3 2.8 1.2 CaO 0.1 0.6 Ta2O5 72.0 70.8 72.5 Na2O 1.3 1.7 2.4 Bi2O3 0.7 0.3 0.6 K2O 0.0 0.05 Sb2O3 13.6 14.2 9.7 Cs2O 7.3 7.4 5.4 SnO 0.1 H2O [1.5] [1.2] PbO 1.6 0.8 5.3 Total 98.9 [99.5] [99.0] (1) Kola Peninsula, Russia; by electron microprobe, average of five analyses; (OH)1− confirmed by IR. (2) Do.; by electron microprobe, H2O calculated from structural considerations; corresponds to [Cs0.31(OH, F)0.69]Σ=1.00(Sb0.57Na0.31Pb0.02Bi0.01)Σ=0.91(Ta1.88Nb0.12)Σ=2.00 [O5.69(OH, F)0.31]Σ=6.00. -
Mineral Commodity Summareis 2013
U.S. Department of the Interior U.S. Geological Survey MINERAL COMMODITY SUMMARIES 2013 Abrasives Fluorspar Mercury Silver Aluminum Gallium Mica Soda Ash Antimony Garnet Molybdenum Sodium Sulfate Arsenic Gemstones Nickel Stone Asbestos Germanium Niobium Strontium Barite Gold Nitrogen Sulfur Bauxite Graphite Peat Talc Beryllium Gypsum Perlite Tantalum Bismuth Hafnium Phosphate Rock Tellurium Boron Helium Platinum Thallium Bromine Indium Potash Thorium Cadmium Iodine Pumice Tin Cement Iron and Steel Quartz Crystal Titanium Cesium Iron Ore Rare Earths Tungsten Chromium Iron Oxide Pigments Rhenium Vanadium Clays Kyanite Rubidium Vermiculite Cobalt Lead Salt Wollastonite Copper Lime Sand and Gravel Yttrium Diamond Lithium Scandium Zeolites Diatomite Magnesium Selenium Zinc Feldspar Manganese Silicon Zirconium U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2013 Manuscript approved for publication January 24, 2013. For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment— visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod For sale by the Superintendent of Documents, U.S. Government Printing Office Mail: Stop IDCC; Washington, DC 20402–0001 Phone: (866) 512–1800 (toll-free); (202) 512–1800 (DC area) Fax: (202) 512–2104 Internet: bookstore.gpo.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. -
A Review of Rare-Element (Li-Cs-Ta) Pegmatite Exploration Techniques for the Superior Province, Canada, and Large Worldwide Tantalum Deposits
Exploration and Mining Geology, Vol. 14, Nos. 1-4, pp. 1-30, 2005 © 2006 Canadian Institute of Mining, Metallurgy and Petroleum. All rights reserved. Printed in Canada. 0964-1823/00 $17.00 + .00 A Review of Rare-Element (Li-Cs-Ta) Pegmatite Exploration Techniques for the Superior Province, Canada, and Large Worldwide Tantalum Deposits JULIE B. SELWAY, FREDERICK W. BREAKS Precambrian Geoscience Section, Ontario Geological Survey 933 Ramsey Lake Road, Sudbury, ON P3E 6B5 ANDREW G. TINDLE Department of Earch Sciences, Open University Milton Keynes, Buckinghamshire, UK MK7 6AA (Received February 16, 2004; accepted September 20, 2004) Abstract — Rare-element pegmatites may host several economic commodities, such as tantalum (Ta- oxide minerals), tin (cassiterite), lithium (ceramic-grade spodumene and petalite), and cesium (pollucite). Key geological features that are common to pegmatites in the Superior province of Ontario and Manitoba, Canada, and in other large tantalum deposits worldwide, can be used in exploration. An exploration project for rare-element pegmatites should begin with an examination of a regional geology map. Rare-element pegmatites occur along large regional-scale faults in greenschist and amphibolite facies metamorphic terranes. They are typically hosted by mafic metavolcanic or metasedimentary rocks, and are located near peraluminous granite plutons (A/CNK > 1.0). Once a peraluminous granite pluton has been identified, then the next step is to determine if the pluton is barren or fertile. Fertile granites have elevated rare element contents, Mg/Li ratio < 10, and Nb/Ta ratio < 8. They commonly contain blocky K-feldspar and green muscovite. Key fractionation indicators can be plotted on a map of the fertile granite pluton to determine the fractionation direction: presence of tourmaline, beryl, and ferrocolumbite; Mn content in garnet; Rb content in bulk K-feldspar; and Mg/Li and Nb/Ta ratios in bulk granite samples. -
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ON POLLUCITE W. E. RrcnMoNDAND F. A. GoNvnn, H araard.U niversi.ty, C ambrid.ge, M ass' 1. POLLUCITE AND PETALITE FROM GREENWOOD,MAINE Introduction Several years ago in the course of feldspar mining at a quarry at the base of Noyes Mountain in Greenwood, Maine, a mineral supposed to be spodumene was found in quantity and about eight tons of it were taken to the grinding mill at West Paris, Maine. There it lay in a bin for a year or more before it was examined by the late W. D' Nevel of Andover, Maine, who identified the mineral as petalite. He sorted out the petalite and the rejects were sacked and retained until the summer of t937. On a visit to the mill that year Richmond selected a quantity of petalite for the Harvard Mineralogical Museum and also carried away some of the waste reject material for examination. This proved, after a delay of months, to contain glassy crystals of pollucite. The effort to securemore of this mineral was unsuccessful,however, sinceon returning to the mill it was found that the lot had been sent through the grinder. Occurrence.The specimensstudied are clearly replacementsof petalite by pollucite and quartz. The pollucite is for the most part massive granular but preserves the laminated structure peculiar to the petalite with which it is associated.Some layers are composed of quartz grains, and elsewhere there are fractures showing indistinct faces of pollucite crystals. In a few cavities in massivepollucite the walls are covered with small crystals of pollucite, the first to be reported from an American locality. -
CHEM 1411 Nomenclature Homework - Answers Part I
1 CHEM 1411 Nomenclature Homework - Answers Part I 1. The following are a list of binary and pseudobinary ionic compounds. Write the name when the formula is given. Write the formula when the name is given. (a) AlCl3 aluminum chloride (k) rubidium oxide Rb2O (b) AuBr3 gold (III) bromide (l) chromium (III) selenide Cr2Se3 (c) Na2S sodium sulfide (m) barium iodide BaI2 (d) Cu3P2 copper (II) phosphide (n) copper (I) fluoride CuF (e) Fe(OH)2 iron (II) hydroxide (o) copper (II) fluoride CuF2 (f) NH4OH ammonium hydroxide (p) strontium cyanide Sr(CN)2 (g) Co(CH3COO)3 cobalt (III) acetate (q) mercury (II) bromide HgBr2 (h) Zn(SCN)2 zinc thiocyanate (r) mercury (I) bromide Hg2Br2 (i) CaCrO4 calcium chromate (s) magnesium permanganate Mg(MnO4)2 (j) K2Cr2O7 potassium dichromate (t) lithium nitride Li3N 2. The following are lists of covalent compounds. Write the name when a formula is given. Write the formula when given a name. (a) CSe2 carbon diselenide (h) dichlorine heptoxide Cl2O7 (b) SF6 sulfur hexafluoride (i) xenon tetrafluoride XeF4 (c) BrF5 bromine pentafluoride (j) carbon monoxide CO (d) P4O10 tetraphosphorous decoxide (k) oxygen O2 (e) Cl2O dichlorine oxide (l) diboron trioxide B2B O3 (f) NH3 ammonia (m) arsenic trifluoride AsF3 (g) N2 dinitrogen or nitrogen (n) diiodine I2 2 3. The following are lists of acids or acid-forming compounds. Write the name when the formula is given. Write the formula when the name is given. (a) H3PO2 hypophosphorous acid (k) hydrogen cyanide HCN (g) (b) H2SO4 sulfuric acid (l) periodic acid HIO4 (c) HClO hypochlorous acid (m) hypochlorous acid HClO (d) H3PO4 phosphoric acid (n) nitric acid HNO3 (e) HBrO4 perbromic acid (o) acetic acid CH3CO2H (f) HIO2 iodous acid (p) chloric acid HClO3 (g) HI (g) hydrogen iodide (q) perbromic acid HBrO4 (h) HI (aq) hydroiodic acid (r) hydrofluoric acid HF (aq) (i) HCN (aq) hydrocyanic acid (s) phosphorous acid H3PO3 (j) HBrO hypobromous acid (t) hydrosulfuric acid H2S (aq) 4. -
AM30 616.Pdf
QUANTITATIVE SPECTROCHEMICAL EXAMINATION OF THE MINOR CONSTITUENTS IN POLLUCITE L. H. AHnnNs, Go o er n m ent M etallur gicaI L abor at or y, W itw ater sr an d U niner s ity, J ohonnesburg, South AJrica. Cor.rrnNrs Introduction. 616 Brief outline of analytical principles. 617 Quantitative analysis of pollucite samples. 618 Discussion: (1) Rubidium and thallium. 619 Quantitative analysis of a lepidolite sample.. 619 (2) Gallium. 620 (3) Lithium. 620 Radioactive disintegration of rubidium. 621 Acknowledgments... 622 References. 622 ABSTRACT Details are given of a quantitative spectrochemical analysis for Tl, Rb, Li, Ga, and K, in two samples of poilucite, one from Karibib, South West Africa, and the other from near Norway, Maine, U.S.A., and the presence of these elements (excluding potassium) within the pollucite lattice is discussed. The ratio, Rb/Tl, is approximately 50 (Karibib) and 180 (Maine). Both ratios are within the limits of 40 and 440 found in 42 analyses of various Rb- and Tl-containing minerals, chiefly South AIrican, data on which will be published later. Although the former ratio (50) is considerably lower than the mean ratio of the 42 analyses (150) it is worth noting that the mean Rb/TI ratio for two samples of lepidolite from the same locality was found to be almost identical (70), providing further evidence that Rb and TI enter different crystal lattices with equal facility. The presence of a trace of strontium is discussed, and a radioactive origin, involving the transition RbE?-51s2, is suggested. h.rrnooucttoN Recently, a sample of pollucite from K.aribib, South West Africa, was examined at the Union Geological Survey, South Africa, by Nel.l This investigation included a qualitative spectrochemicalanalysis by Dr. -
The Preparation and Identification of Rubidium
THE PREPARATION AND IDENTIFICATION OF RUBIDIUM TELLURO-MOLYBDATE AND OF CESIIDl TELLURO- MOLYBDA.TE SEP ZI 193B THE PREPARATION AlJD IDENTIFICATION or :RUBIDIUM TELLURO-MOLYBDATE AND OF CESIUM '?ELLURO-MOLYBDATE By HENRY ARTHUR CARLSON \ \ Bachelor of Science Drury College Springfield. Missouri 1936 Submitted to the Department of Chemistry Oklahoma Agricultural and Meohanica.l College In Partial Fulfillment of the Requirements For the degree of MASTER OF SCIENCE 1938 . ... ... .. .. .. ... .. ' :· ·. : : . .. .. ii S£p C"·J"··} ;.;:{ I' ' """"''· APPROVED:- \ Head~~stry 108627 iii ACKNOWLEDGMENT The author wishes to acknowledge the valuabl e advice and assistance of Dr. Sylvan R~ Wood, under whose direction this work was done. Acknowledgment is also made of the many help ful suggestions and cordial cooperation of Dr. H. M. Trimble. The author wishes to express his sincere appreciation to the Oklahoma Agricultural and Mechanical College for financial assistance in the fonn of a graduate assistantship in the Depart ment of Chemistry during the school years 1936-37 and 1937-38. iv TABLE OF CONTENTS I. Introduction------------------------------ 1 II. Materials Used-------------"--------------- 3 III. Preparation of Rubidium Telluro-molybdate---- 5 IV. Methods of Analysis------------------------ 6 Telluriur a-"---------"----------------------- 6 Molybdenum•----------------------------- 8 Rubi di um------------------"-------------... 10 \Yater of Hydration---------------------- 11 v. Calculation of: Formula---------------------- 12 VI. Preparation -
New Family of Silicate Phases with the Pollucite Structure
Zeitschrift fUr Kristallographie 175, 1-7 (1986) @ by R. Oldenbourg Verlag, Miinchen 1986 New family of silicate phases with the pollucite structure Leticia M. Torres-Martinez and A. R. West University of Aberdeen, Department of Chemistry, Meston Walk, Old Aberdeen AB9 2UE, Scotland, United Kingdom Received: April 10, 1984; in final form: February 14, 1986 Pollucite structure I RbzMgSis012 type Abstract. A new family of silicate phases, CszMSi5012: M = Be, Mg, Fe, Co, Ni, Zn, Cd; RbzMSi5012: M = Mg, Fe, (Co, Zn) has been prepared with the cubic pollucite structure, a in the range 13.3 to 13.8 A, space group Ia3d, Z = 8. The structure of one, RbzMgSi5012' has been refined to R = 10.8% using X-ray powder data. The structures are built of a 3D, [MSi50u]z- framework containing large, 12-coordinated cavities for the alkali cations. These structures are unusual in that a wide range of divalent cations have partially replaced Si4+ in the silicate anion framework. Introduction Pollucite, CsAISiz06, is a framework alumino silicate containing large, 12- coordinated cavities suitable for occupation by Cs+ ions (Strunz, 1936; Naray-Szabo, 1938; Newnham, 1967). The unit cell is cubic with space group Ia3d, Z = 16. Similar alumino-silicate frameworks are present in analcite, NaAISiz06 . HzO and leucite, KAISiz06 (Taylor, 1938; Beattie, 1954; Knowles et aI., 1965; Wyart, 1941; Deer et aI., 1963; Wyckoff, 1968), although leucite is tetragonal below 6050 (Wyart, 1941; Deer et aI., 1963; Wyckoff, 1968). Structural studies on these phases are complicated by the occurrence of twinning in tetragonalleucite (Mazzi et aI., 1976) and by Si, Al disorder in the alumino silicate framework. -
Chemical Names and CAS Numbers Final
Chemical Abstract Chemical Formula Chemical Name Service (CAS) Number C3H8O 1‐propanol C4H7BrO2 2‐bromobutyric acid 80‐58‐0 GeH3COOH 2‐germaacetic acid C4H10 2‐methylpropane 75‐28‐5 C3H8O 2‐propanol 67‐63‐0 C6H10O3 4‐acetylbutyric acid 448671 C4H7BrO2 4‐bromobutyric acid 2623‐87‐2 CH3CHO acetaldehyde CH3CONH2 acetamide C8H9NO2 acetaminophen 103‐90‐2 − C2H3O2 acetate ion − CH3COO acetate ion C2H4O2 acetic acid 64‐19‐7 CH3COOH acetic acid (CH3)2CO acetone CH3COCl acetyl chloride C2H2 acetylene 74‐86‐2 HCCH acetylene C9H8O4 acetylsalicylic acid 50‐78‐2 H2C(CH)CN acrylonitrile C3H7NO2 Ala C3H7NO2 alanine 56‐41‐7 NaAlSi3O3 albite AlSb aluminium antimonide 25152‐52‐7 AlAs aluminium arsenide 22831‐42‐1 AlBO2 aluminium borate 61279‐70‐7 AlBO aluminium boron oxide 12041‐48‐4 AlBr3 aluminium bromide 7727‐15‐3 AlBr3•6H2O aluminium bromide hexahydrate 2149397 AlCl4Cs aluminium caesium tetrachloride 17992‐03‐9 AlCl3 aluminium chloride (anhydrous) 7446‐70‐0 AlCl3•6H2O aluminium chloride hexahydrate 7784‐13‐6 AlClO aluminium chloride oxide 13596‐11‐7 AlB2 aluminium diboride 12041‐50‐8 AlF2 aluminium difluoride 13569‐23‐8 AlF2O aluminium difluoride oxide 38344‐66‐0 AlB12 aluminium dodecaboride 12041‐54‐2 Al2F6 aluminium fluoride 17949‐86‐9 AlF3 aluminium fluoride 7784‐18‐1 Al(CHO2)3 aluminium formate 7360‐53‐4 1 of 75 Chemical Abstract Chemical Formula Chemical Name Service (CAS) Number Al(OH)3 aluminium hydroxide 21645‐51‐2 Al2I6 aluminium iodide 18898‐35‐6 AlI3 aluminium iodide 7784‐23‐8 AlBr aluminium monobromide 22359‐97‐3 AlCl aluminium monochloride -
Paper Number: 2059
Paper Number: 2059 New Geochronological, Isotopic and Fluid Inclusion Study Constraints on the Formation of the World-class Bikita LCT Pegmatite Deposit Dittrich, T.1, Seifert, T.1, Richter, L.1, Hagemann, S.2, Lüders, V.3, Schulz, B.1, Pfänder, J.A.4 and Gerdes, A.5 1Division of Economic Geology and Petrology, TU Bergakademie Freiberg/Germany [email protected] freiberg.de 2University of Western Australia, Centre for Exploration Targeting, Crawley/Australia 3Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Potsdam/Germany 4ArgonLab Freiberg, Department of Geology, TU Bergakademie Freiberg/Germany 5Institute for Geosciences, Goethe University, Frankfurt am Main/Germany ___________________________________________________________________________________________ The increasing demand for metals such as Li and Ta used by high technology applications (e.g., renewable energies, electronics) led to increasing exploration activities on lithium-cesium-tantalum (LCT) pegmatite deposits worldwide. LCT pegmatites are interpreted to be linked to granitic systems and represent the geochemically most enriched, highest fractionated portions of initially granitic melts and thus can host economic quantities of various metals (i.e., Li, Cs, Ta, Nb, Sn, Rb, Be). However, many economic LCT pegmatite deposits (e.g., Tanco/Canada, Greenbushes, Wodgina/Western Australia) are situated in greenstone belt successions on Archean Cratons making those prospective exploration areas [1]. The Bikita LCT pegmatite deposit located in the Zimbabwe Craton represents a typical example of Archean LCT pegmatites. The pegmatites are hosted by metavolcanic rocks of the Masvingo greenstone belt [2] and represent the highest evolved portions of a 20 km long NE-SW striking pegmatite field. The Bikita pegmatite is currently mined for Li (petalite) and Cs (pollucite). -
The Crystal Structure and Chemical Composition of Pollucite
Zeitschrift fUr Kristallographie, Bd. 129, S. 280-302 (1969) The crystal structure and chemical composition of pollucite By RICHARD M. BEGER * (Received May 20, 1968) Crystallographic Laboratory, Massachusetts Institute of Technology Cambridge, Massachusetts Auszug Die Struktur des Pollucits von Rumford, Maine, wurde aus 213, mit einem Diffraktometer gemessenen Interferenzen bestimmt und bis R = 0,050 fiir aIle Interferenzen verfeinert. Raumgruppe ist Ia3d, Gitterkonstante a = 13,69 A. Das Strukturgeriist ist das gleiche wie beim Analcim. Die gro13en Hohlriiume sind von Caesiumatomen und Wassermolekiilen besetzt. Die Natriumatome befinden sich wie beim Analcim in der Punktlage 24c, [t to]. Sie sind jedoch in groJ3eren, von Wassermolekiilen begrenzten Gruppen nach Zufall angesam- melt. Die allgemeine Zusammensetzung des Pollucits liiJ3t sich durch eine y Formel von der Art CsxNayAlx+ySi4s-x-y096 . (16-x) H20 mit 2y :> 16 - x :> ausdriicken. Abstract The structure of pollucite from Rumford, Maine has been determined and refined. The space group is Ia3d with cell edge a = 13.69 A. The structure was investigated using 213 independent reflection intensities measured on a single crystal diffractometer. Pollucite has the analcime framework with the cesium atoms occupying the large voids in the framework, as initially suggested by NARAY-SZABO. The water molecules occupy the large voids of this same set which are not occupied by the cesium atoms. The sodium atoms are located in equipoint 24c, at t t 0, in the positions between the water molecules. The water molecules and the sodium atoms occupy the same positions as they do in analcime, but they occur only in randomly distributed clusters of atoms whose outer members are restricted to water molecules.